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{{About|the current and projected rise in the world's average sea level|sea level rise in general|Past sea level}}

<noinclude>[[File:1880- Global average sea level rise (SLR) - annually.svg |thumb|upright=1.35 |The global average sea level has risen about {{convert|250|mm|in}} since 1880.<ref name=EPA_SLR_202207>{{cite web |title=Climate Change Indicators: Sea Level / Figure 1. Absolute Sea Level Change |url=https://www.epa.gov/climate-indicators/climate-change-indicators-sea-level |website=EPA.gov |publisher=U.S. Environmental Protection Agency (EPA) |archive-url=https://web.archive.org/web/20230904035800/https://www.epa.gov/climate-indicators/climate-change-indicators-sea-level |archive-date=4 September 2023 |date=July 2022 |quote=Data sources: CSIRO, 2017. NOAA, 2022. |url-status=live}}</ref>]]</noinclude>

<noinclude>[[File:Sea surface height change from 1992 to 2019.webm|thumb|upright=1.35| {{center|Sea surface height change from 1992 to 2019 – NASA}} The visualization is based on data collected from the TOPEX/Poseidon, Jason-1, Jason-2, and Jason-3 satellites. Blue regions are where sea level has gone down, and orange/red regions are where sea level has risen.<ref name="NASA2020">[https://svs.gsfc.nasa.gov/4853 27-year Sea Level Rise – TOPEX/JASON] ''NASA Visualization Studio'', 5 November 2020. {{PD-notice}}</ref>]]</noinclude>

<noinclude>[[File:20210125 The Cryosphere - Floating and grounded ice - imbalance - climate change.png|thumb|upright=1.5|Earth lost 28&nbsp;trillion tonnes of ice between 1994 and 2017: ice sheets and glaciers raised the global sea level by 34.6 ± 3.1 mm. The rate of ice loss has risen by 57% since the 1990s−from 0.8 to 1.2&nbsp;trillion tonnes per year.<ref name=Cryosphere20210125>{{cite journal |last1=Slater |first1=Thomas |last2=Lawrence |first2=Isobel R. |last3=Otosaka |first3=Inès N. |last4=Shepherd |first4=Andrew |last5=Gourmelen |first5=Noel |last6=Jakob |first6=Livia |last7=Tepes |first7=Paul |last8=Gilbert |first8=Lin |last9=Nienow |first9=Peter |display-authors=4 |title=Review article: Earth's ice imbalance |journal=The Cryosphere |date=25 January 2021 |volume=15 |issue=1 |pages=233–246 |doi=10.5194/tc-15-233-2021 |bibcode=2021TCry...15..233S |s2cid=234098716 |url=https://tc.copernicus.org/articles/15/233/2021/ |language=English |issn=1994-0416 |doi-access=free}} Fig. 4.</ref>|alt=A graph showing ice loss sea ice, ice shelves and land ice. Land ice loss contributes to SLR]]</noinclude>

Between 1901 and 2018, the average global '''sea level rise''' was {{cvt|15|–|25|cm|in|frac=2}}, with an increase of {{convert|2.3|mm|abbr=on}} per year since the 1970s.<ref name="IPCC AR6 WG1 Ch.9" />{{rp|1216}} This is faster than the [[sea level]] has risen over the past 3,000 years, if not longer.<ref name="IPCC AR6 WG1 Ch.9" />{{rp|1216}} The rate accelerated to {{convert|4.62|mm|abbr=on}}/yr for the decade 2013–2022.<ref name=WMO_20230421/> [[Climate change]] due to human activities is the main cause.<ref name="IPCC_2021_WGI_SPM" />{{rp|5,8}} Between 1993 and 2018, melting [[ice sheets]] and [[Glacier|glaciers]] accounted for 44% of sea level rise, with another 42% resulting from [[thermal expansion]] of [[water]].<ref name="WCRP2018">{{cite journal |author=WCRP Global Sea Level Budget Group |year=2018 |title=Global sea-level budget 1993–present |journal=Earth System Science Data |volume=10 |issue=3 |pages=1551–1590 |bibcode=2018ESSD...10.1551W |doi=10.5194/essd-10-1551-2018 |quote=This corresponds to a mean sea-level rise of about 7.5 cm over the whole altimetry period. More importantly, the GMSL curve shows a net acceleration, estimated to be at 0.08mm/yr2. |doi-access=free}}</ref>{{Rp|1576}}

Sea level rise lags behind changes in the [[Earth]]'s temperature, and sea level rise will therefore continue to accelerate between now and 2050 in response to warming that has already happened.<ref name="us nrc 2011 long term slr">{{cite book |author=((National Academies of Sciences, Engineering, and Medicine)) |year=2011 |quote=Box SYN-1: Sustained warming could lead to severe impacts |chapter-url=https://nap.nationalacademies.org/read/12877/chapter/3 |page=[https://nap.nationalacademies.org/read/12877/chapter/3#5 5] |chapter=Synopsis |title=Climate Stabilization Targets: Emissions, Concentrations, and Impacts over Decades to Millennia |location=Washington, DC |publisher=The National Academies Press |doi=10.17226/12877|isbn=978-0-309-15176-4}}</ref> What happens after that depends on human [[greenhouse gas emissions]]. Sea level rise would slow between 2050 and 2100 if there are very deep cuts in emissions. It could then reach slightly over {{cvt|30|cm|ft|frac=2}} from now by 2100. With high emissions it would accelerate. It could rise by {{cvt|1.01|m|ft|frac=3}} or even {{cvt|1.6|m|ft|frac=3}} by then.<ref name="IPCC_2021_WGI_SPM" /><ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1302}} In the long run, sea level rise would amount to {{convert|2-3|m|ft|0|abbr=on}} over the next 2000 years if warming amounts to {{convert|1.5|C-change|F-change}}. It would be {{convert|19-22|m|ft}} if warming peaks at {{convert|5|C-change|F-change}}.<ref name="IPCC_2021_WGI_SPM">IPCC, 2021: [https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_SPM.pdf Summary for Policymakers]. In: [https://www.ipcc.ch/report/ar6/wg1/ Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change] Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M. I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J. B. R. Matthews, T. K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.). Cambridge University Press, Cambridge, United Kingdom and New York, New York, US, pp. 3−32, doi:10.1017/9781009157896.001.</ref>{{rp|21}}

Rising seas affect every coastal and island population on Earth.<ref>{{Cite journal|last1=McMichael|first1=Celia|last2=Dasgupta|first2=Shouro|last3=Ayeb-Karlsson|first3=Sonja|last4=Kelman|first4=Ilan|date=2020-11-27 |title=A review of estimating population exposure to sea-level rise and the relevance for migration|journal=Environmental Research Letters|volume=15|issue=12|page=123005|doi=10.1088/1748-9326/abb398|pmid=34149864|pmc=8208600|bibcode=2020ERL....15l3005M|issn=1748-9326}}</ref><ref name="wg1-5-5-1">{{cite book |author=Bindoff |first1=N. L. |title=Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change |last2=Willebrand |first2=J. |last3=Artale |first3=V. |last4=Cazenave |first4=A. |last5=Gregory |first5=J. |last6=Gulev |first6=S. |last7=Hanawa |first7=K. |last8=Le Quéré |first8=C. |last9=Levitus |first9=S. |date=2007 |isbn=978-0-521-88009-1 |editor=Solomon |editor-first=S. |language=en |chapter=Observations: Ocean Climate Change and Sea Level: §5.5.1: Introductory Remarks |author4-link=Anny Cazenave |access-date=25 January 2017 |editor2=Qin |editor-first2=D. |editor3=Manning |editor-first3=M. |editor4=Chen |editor-first4=Z. |editor5=Marquis |editor-first5=M. |editor6=Averyt |editor-first6=K. B. |editor7=Tignor |editor-first7=M. |editor8=Miller |editor-first8=H. L. |chapter-url=http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch5s5-5.html#5-5-1 |archive-url=https://web.archive.org/web/20170620210108/http://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch5.html |archive-date=20 June 2017 |author10=Nojiri, Y. |author11=Shum, C. K. |author12=Talley, L. D. |author13=Unnikrishnan, A.|publisher=Cambridge University Press}}</ref> This can be through flooding, higher [[storm surge]]s, [[king tide]]s, and [[tsunami]]s. There are many knock-on effects. They lead to loss of coastal [[ecosystem]]s like [[mangroves]]. [[Crop yield|Crop yields]] may reduce because of [[Freshwater salinization|increasing salt levels]] in [[irrigation]] water. Damage to ports disrupts sea trade.<ref name="IPCC-2001" /><ref name="UPI-2018">{{cite web |year=2018 |title=Sea level to increase risk of deadly tsunamis |url=https://www.upi.com/Science_News/2018/08/15/Sea-level-to-increase-risk-of-deadly-tsunamis/2361534362716/ |website=United Press International}}</ref><ref name="Holder-2017" /> The sea level rise projected by 2050 will expose places currently inhabited by tens of millions of people to annual flooding. Without a sharp reduction in greenhouse gas emissions, this may increase to hundreds of millions in the latter decades of the century.<ref name="Kulp2019" /> Areas not directly exposed to rising sea levels could be vulnerable to large-scale migration and economic disruption.

Local factors like [[tidal range]] or land [[subsidence]] will greatly affect the severity of impacts. There is also the varying resilience and [[Climate change adaptation|adaptive capacity]] of ecosystems and countries which will result in more or less pronounced impacts.<ref>{{Cite journal|last=Mimura|first=Nobuo|date=2013|title=Sea-level rise caused by climate change and its implications for society|journal=Proceedings of the Japan Academy. Series B, Physical and Biological Sciences|volume=89|issue=7|pages=281–301|doi=10.2183/pjab.89.281|issn=0386-2208|pmc=3758961|pmid=23883609|bibcode=2013PJAB...89..281M}}</ref> For instance, [[sea level rise in the United States]] (particularly along the [[US East Coast]]) is likely to be 2 to 3 times greater than the global average by the end of the century.<ref>{{cite web |last1=Choi |first1=Charles Q. |date=27 June 2012|title=Sea Levels Rising Fast on U.S. East Coast |url=https://www.nationalgeographic.com/science/article/120625-sea-level-rise-east-coast-us-science-nature-climate-change |archive-url=https://web.archive.org/web/20210504002931/https://www.nationalgeographic.com/science/article/120625-sea-level-rise-east-coast-us-science-nature-climate-change |archive-date=May 4, 2021 |access-date=October 22, 2022 |website=National Oceanic and Atmospheric Administration}}</ref><ref name="NOAA-2022">{{Cite web |title=2022 Sea Level Rise Technical Report |url=https://oceanservice.noaa.gov/hazards/sealevelrise/sealevelrise-tech-report.html |access-date=2022-07-04 |website=oceanservice.noaa.gov |language=EN-US}}</ref> Yet, of the 20 countries with the greatest exposure to sea level rise, 12 are in [[Asia]], including [[Indonesia]], [[Bangladesh]] and the Philippines.<ref name="AR6_WGII_Chapter10" /> The greatest [[Effects of climate change on humans|impact on human populations]] in the near term will occur in the low-lying [[Caribbean]] and [[Pacific islands]]. Sea level rise will make many of them uninhabitable later this century.<ref name="AR6_WGII_Chapter15">Mycoo, M., M. Wairiu, D. Campbell, V. Duvat, Y. Golbuu, S. Maharaj, J. Nalau, P. Nunn, J. Pinnegar, and O. Warrick, 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_Chapter15.pdf Chapter 15: Small islands]. In [https://www.ipcc.ch/report/ar6/wg2/ Climate Change 2022: Impacts, Adaptation and Vulnerability] [H.-O. Pörtner, D. C. Roberts, M. Tignor, E. S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, New York, US, pp. 2043–2121 |doi=10.1017/9781009325844.017.</ref>

Societies can adapt to sea level rise in multiple ways. [[Managed retreat]], [[Coastal management|accommodating coastal change]], or protecting against sea level rise through hard-construction practices like [[seawall]]s<ref>{{cite web |year=2013 |title=IPCC's New Estimates for Increased Sea-Level Rise |url=http://www.yaleclimateconnections.org/2013/10/ipccs-new-estimates-for-increased-sea-level-rise/ |publisher=Yale University Press}}</ref> are hard approaches. There are also soft approaches such as [[Sand dune stabilization|dune rehabilitation]] and [[beach nourishment]]. Sometimes these adaptation strategies go hand in hand. At other times choices must be made among different strategies.<ref name="Thomsen-2012">{{Cite journal |last1=Thomsen |first1=Dana C. |last2=Smith |first2=Timothy F. |last3=Keys |first3=Noni |date=2012 |title=Adaptation or Manipulation? Unpacking Climate Change Response Strategies |journal=Ecology and Society |volume=17 |issue=3 |doi=10.5751/es-04953-170320 |jstor=26269087 |doi-access=free}}</ref> A managed retreat strategy is difficult if an area's population is increasing rapidly. This is a particularly acute problem for [[Africa]].<ref name="AR6_WGII_Chapter9">Trisos, C. H., I. O. Adelekan, E. Totin, A. Ayanlade, J. Efitre, A. Gemeda, K. Kalaba, C. Lennard, C. Masao, Y. Mgaya, G. Ngaruiya, D. Olago, N. P. Simpson, and S. Zakieldeen 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_Chapter09.pdf Chapter 9: Africa]. In [https://www.ipcc.ch/report/ar6/wg2/ Climate Change 2022: Impacts, Adaptation and Vulnerability] [H.-O. Pörtner, D.C. Roberts, M. Tignor, E. S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, New York, US, pp. 2043–2121 |doi=10.1017/9781009325844.011.</ref> Poorer nations may also struggle to implement the same approaches to adapt to sea level rise as richer states. Sea level rise at some locations may be compounded by other environmental issues. One example is [[subsidence]] in [[sinking cities]].<ref>{{Cite journal|last1=Nicholls|first1=Robert J.|last2=Marinova|first2=Natasha|last3=Lowe|first3=Jason A.|last4=Brown|first4=Sally|last5=Vellinga|first5=Pier|last6=Gusmão|first6=Diogo de|last7=Hinkel|first7=Jochen|last8=Tol|first8=Richard S. J.|date=2011|title=Sea-level rise and its possible impacts given a 'beyond 4°C (39.2°F)world' in the twenty-first century|journal=Philosophical Transactions of the Royal Society of London A: Mathematical, Physical and Engineering Sciences|volume=369|issue=1934|pages=161–181|doi=10.1098/rsta.2010.0291|issn=1364-503X|pmid=21115518|bibcode=2011RSPTA.369..161N|s2cid=8238425|doi-access=free}}</ref> [[Marine coastal ecosystem|Coastal ecosystems]] typically adapt to rising sea levels by moving inland. Natural or artificial barriers may make that impossible.<ref name="birdlife-2015" />
{{TOC level|3}}

== Observations ==
Between 1901 and 2018, the global mean sea level rose by about {{convert|20|cm|abbr=on}}.<ref name="IPCC_2021_WGI_SPM" /> More precise data gathered from satellite [[radar]] measurements found an increase of {{convert|7.5|cm|abbr=on}} from 1993 to 2017 (average of {{convert|2.9|mm|abbr=on}}/yr).<ref name="WCRP2018" /> This accelerated to {{convert|4.62|mm|abbr=on}}/yr for 2013–2022.<ref name="WMO_20230421">{{cite web |date=21 April 2023 |title=WMO annual report highlights continuous advance of climate change |url=https://wmo.int/news/media-centre/wmo-annual-report-highlights-continuous-advance-of-climate-change |publisher=World Meteorological Organization |quote=Press Release Number: 21042023.}}</ref> [[Paleoclimate]] data shows that this rate of sea level rise is the fastest it had been over at least the past 3,000 years.<ref name="IPCC AR6 WG1 Ch.9" />{{rp|1216}}

=== Regional variations ===
{{Further|Relative sea level|Sinking cities}}
[[File:Ohenhen 2023 EC subsidence.png|thumb|Sea level rise in many locations across the world is worsened due to land subsidence, and East Coast of the United States is one example<ref>{{Cite journal |last1=Ohenhen |first1=Leonard O. |last2=Shirzaei |first2=Manoochehr |last3=Ojha |first3=Chandrakanta |last4=Kirwan |first4=Matthew L. |date=11 April 2023 |title=Hidden vulnerability of US Atlantic coast to sea-level rise due to vertical land motion |journal=Nature Communications |volume=14 |issue=1 |page=2038 |doi=10.1038/s41467-023-37853-7 |pmid=37041168 |pmc=10090057 |bibcode=2023NatCo..14.2038O}}</ref>]]

Sea level rise is not uniform around the globe. Some land masses are moving up or down as a consequence of [[subsidence]] (land sinking or settling) or [[post-glacial rebound]] (land rising as melting ice reduces weight). Therefore, local relative sea level rise may be higher or lower than the global average. Changing ice masses also affect the distribution of sea water around the globe through gravity.<ref>{{Cite journal |last1=Katsman |first1=Caroline A. |last2=Sterl |first2=A. |last3=Beersma |first3=J. J. |last4=van den Brink |first4=H. W. |last5=Church |first5=J. A. |last6=Hazeleger |first6=W. |last7=Kopp |first7=R. E. |last8=Kroon |first8=D. |last9=Kwadijk |first9=J. |date=2011 |title=Exploring high-end scenarios for local sea level rise to develop flood protection strategies for a low-lying delta—the Netherlands as an example |journal=Climatic Change |volume=109 |issue=3–4 |pages=617–645 |doi=10.1007/s10584-011-0037-5 |issn=0165-0009 |doi-access=free |s2cid=2242594}}</ref><ref name="ipcc13">{{cite book |last1=Church |first1=J. A. |title=Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change |last2=Clark |first2=P. U. |publisher=Cambridge University Press |year=2013 |editor-last=Stocker |editor-first=T. F. |location=Cambridge, United Kingdom and New York, New York, US |chapter=Sea Level Change |display-editors=etal |chapter-url=https://ipcc.ch/report/ar5/wg1/}}</ref>

When a glacier or ice sheet melts, it loses mass. This reduces its gravitational pull. In some places near current and former glaciers and ice sheets, this has caused water levels to drop. At the same time water levels will increase more than average further away from the ice sheet. Thus ice loss in [[Greenland]] affects regional sea level differently than the equivalent loss in [[Antarctica]].<ref name="Rovere-2016">{{cite journal |last1=Rovere |first1=Alessio |last2=Stocchi |first2=Paolo |last3=Vacchi |first3=Matteo |date=2 August 2016 |title=Eustatic and Relative Sea Level Changes |journal=Current Climate Change Reports |volume=2 |issue=4 |pages=221–231 |doi=10.1007/s40641-016-0045-7 |bibcode=2016CCCR....2..221R |doi-access=free |s2cid=131866367}}</ref> On the other hand, the Atlantic is warming at a faster pace than the Pacific. This has consequences for Europe and the [[U.S. East Coast]]. The East Coast sea level is rising at 3–4 times the global average.<ref>{{cite news |year=2016 |title=Why the U.S. East Coast could be a major 'hotspot' for rising seas |newspaper=The Washington Post |url=https://www.washingtonpost.com/news/energy-environment/wp/2016/02/01/why-the-u-s-east-coast-could-be-a-major-hotspot-for-sea-level-rise/}}</ref> Scientists have linked extreme regional sea level rise on the US Northeast Coast to the downturn of the [[Atlantic meridional overturning circulation]] (AMOC).<ref>{{cite news |last1=Yin |first1=Jianjun |last2=Griffies |first2=Stephen |name-list-style=amp |date=March 25, 2015 |title=Extreme sea level rise event linked to AMOC downturn |url=https://usclivar.org/research-highlights/extreme-sea-level-rise-event-linked-amoc-downturn |publisher=CLIVAR}}</ref>

Many [[port]]s, urban conglomerations, and agricultural regions stand on [[river delta]]s. Here land subsidence contributes to much higher [[Relative sea level|''relative'' sea level]] rise. Unsustainable extraction of [[groundwater]] and oil and gas is one cause. [[Levee]]s and other flood management practices are another. They prevent sediments from accumulating. These would otherwise compensate for the natural settling of deltaic soils.<ref>{{Cite journal |last1=Tessler |first1=Z. D. |last2=Vörösmarty |first2=C. J. |last3=Grossberg |first3=M. |last4=Gladkova |first4=I. |last5=Aizenman |first5=H. |last6=Syvitski |first6=J. P. M. |last7=Foufoula-Georgiou |first7=E. |date=2015-08-07 |title=Profiling risk and sustainability in coastal deltas of the world |url=https://cloudfront.escholarship.org/dist/prd/content/qt46n8t5mp/qt46n8t5mp.pdf |journal=Science |volume=349 |issue=6248 |pages=638–643 |doi=10.1126/science.aab3574 |issn=0036-8075 |pmid=26250684|bibcode=2015Sci...349..638T |s2cid=12295500}}</ref>{{rp|638}}<ref name="Bucx 2010">{{cite book |last=Bucx |first=Tom |title=Comparative assessment of the vulnerability and resilience of 10 deltas: synthesis report |date=2010 |publisher=Deltares |isbn=978-94-90070-39-7 |publication-place=Delft, Netherlands |oclc=768078077}}</ref>{{rp|88}} Estimates for total human-caused subsidence in the [[Rhine-Meuse-Scheldt delta]] (Netherlands) are {{Cvt|3-4|m|ft|0}}, over {{Cvt|3|m|ft|0}} in urban areas of the [[Mississippi River Delta]] ([[New Orleans]]), and over {{Cvt|9|m|ft|0}} in the [[Sacramento–San Joaquin River Delta]].<ref name="Bucx 2010" />{{rp|81–90}} On the other hand, relative sea level around the [[Hudson Bay]] in [[Canada]] and the northern [[Baltic Sea]] is falling due to post-glacial isostatic rebound.<ref>{{Cite journal |last1=Cazenave |first1=Anny |author-link=Anny Cazenave |last2=Nicholls |first2=Robert J. |date=2010 |title=Sea-Level Rise and Its Impact on Coastal Zones |journal=Science |volume=328 |issue=5985 |pages=1517–1520 |bibcode=2010Sci...328.1517N |doi=10.1126/science.1185782 |issn=0036-8075 |pmid=20558707 |s2cid=199393735}}</ref>

== Projections ==
[[File:Slangen 2022 8 SLRs.jpg|thumb|left|Sea level rise for the low-emission, high-emission (RCP 8.5, lower left) and in-between scenarios according to the different approaches. Projections are very similar for low warming, but disagreement increases alongside the temperature<ref name="Slangen2022" />]]
Several approaches are used for sea level rise (SLR) projections.<ref name="Slangen2022" /> One is process-based modeling, where ice melting is computed through an [[ice-sheet model]] and rising sea temperature and expansion through a [[general circulation model]], and then these contributions are added up.<ref name="Moore2013">{{cite journal |last1=Moore |first1=John C. |last2=Grinsted |first2=Aslak |last3=Zwinger |first3=Thomas |last4=Jevrejeva |first4=Svetlana |date=10 June 2013 |title=Semiempirical and process-based global sea level projections |journal=Reviews of Geophysics |volume=51 |issue=3 |page=484-522 |doi=10.1002/rog.20015 |bibcode=2013RvGeo..51..484M}}</ref> The so-called semi-empirical approach applies statistical techniques and basic physical modeling to the observed sea level rise and its reconstructions from the historical geological data (known as [[paleoclimate]] modelling).<ref name="Mengel2016" /> It was developed because model projections in the past IPCC reports (such as the [[Fourth Assessment Report]] from 2007) were found to underestimate the already observed sea level rise.<ref name="Moore2013" />

By 2013, improvements in modelling had addressed this issue, and model and semi-empirical projections for the year 2100 are now very similar.<ref name="Moore2013" /><ref name="Slangen2022" /> Yet, semi-empirical estimates are reliant on the quality of available observations and struggle to represent non-linearities, while processes without enough available information about them cannot be modelled.<ref name="Moore2013" /> Thus, another approach is to combine the opinions of a large number of scientists in what is known as a structured expert judgement (SEJ).<ref name="Slangen2022" />

Variations of these primary approaches exist.<ref name="Slangen2022" /> For instance, large climate models are always in demand, so less complex models are often used in their place for simpler tasks like projecting flood risk in the specific regions. A structured expert judgement may be used in combination with modelling to determine which outcomes are more or less likely, which is known as "shifted SEJ". Semi-empirical techniques can be combined with the so-called "intermediate-complexity" models.<ref name="Slangen2022" /> After 2016, some ice sheet modelling exhibited the so-called ice cliff instability in Antarctica, which results in substantially faster disintegration and retreat than normally simulated.<ref name="DeConto2016">{{Cite journal |last1=DeConto |first1=Robert M. |last2=Pollard |first2=David |date=30 March 2016 |title=Contribution of Antarctica to past and future sea-level rise |journal=Nature |language=en |volume=531 |issue=7596 |pages=591–597 |doi=10.1038/nature17145 |pmid=27029274 |bibcode=2016Natur.531..591D |s2cid=205247890}}</ref><ref>{{cite news |last=Gillis |first=Justin |date=30 March 2016 |title=Climate Model Predicts West Antarctic Ice Sheet Could Melt Rapidly |newspaper=The New York Times |url=https://www.nytimes.com/2016/03/31/science/global-warming-antarctica-ice-sheet-sea-level-rise.html}}</ref> The differences are limited with low warming, but at higher warming levels, ice cliff instability simulates far greater sea level rise than any other approach.<ref name="Slangen2022">{{cite journal |last1=Slangen |first1=A. B. A. |last2=Haasnoot |first2=M. |last3=Winter |first3=G. |date=30 March 2022 |title=Rethinking Sea-Level Projections Using Families and Timing Differences |journal=Earth's Future |volume=10 |issue=4 |page=e2021EF002576 |doi=10.1029/2021EF002576 |bibcode=2022EaFut..1002576S |url=https://www.vliz.be/imisdocs/publications/00/378000.pdf}}</ref>

=== Projections for the 21st century ===
[[File:Sea level history and projections.svg|thumb|right|upright=1.35|Historical sea level reconstruction and projections up to 2100 published in 2017 by the [[U.S. Global Change Research Program]].<ref name="NOAA-2017">{{Cite web|url=https://tidesandcurrents.noaa.gov/publications/techrpt83_Global_and_Regional_SLR_Scenarios_for_the_US_final.pdf|title=January 2017 analysis from NOAA: Global and Regional Sea Level Rise Scenarios for the United States}}</ref> RCPs are different scenarios for future concentrations of greenhouse gases.]]
[[Intergovernmental Panel on Climate Change]] is the largest and most influential scientific organization on climate change, and since 1990, it provides several plausible scenarios of 21st century sea level rise in each of its major reports. The differences between scenarios are mainly due to uncertainty about future [[greenhouse gas]] emissions. These depend on future economic developments, and also future political action which is hard to predict. Each scenario provides an estimate for sea level rise as a range with a lower and upper limit to reflect the unknowns. The scenarios in the 2013–2014 [[Fifth Assessment Report]] (AR5) were called [[Representative Concentration Pathway]]s, or RCPs and the scenarios in the [[IPCC Sixth Assessment Report]] (AR6) are known as [[Shared Socioeconomic Pathways]], or SSPs. A large difference between the two was the addition of SSP1-1.9 to AR6, which represents meeting the best [[Paris climate agreement]] goal of {{convert|1.5|C-change|F-change}}. In that case, the likely range of sea level rise by 2100 is {{cvt|28–55|cm|in|frac=2}}.<ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1302}}
[[File:Kopp 2023 4 flows.png|thumb|upright=1.35|left|For the 2021 IPCC report, three steps were taken to present a wider picture than the previous report (top left): state-of-the-art [[ice sheet model]] projections from 2020 (lower left), research modelling the possibility of ice cliff instability (upper right) and combined expert projections of sea level rise from Greenland and Antarctica (lower right) were all considered before settling on the projections. Note that projections on the right use a larger scale, which ends at {{cvt|2.5|m|ft|frac=3}} instead of {{cvt|1.5|m|ft|frac=3}}<ref name="Kopp2023" /> ]]
The lowest scenario in AR5, RCP2.6, would see greenhouse gas emissions low enough to meet the goal of limiting warming by 2100 to {{convert|2|C-change|F-change}}. It shows sea level rise in 2100 of about {{convert|44|cm|abbr=on}} with a range of {{convert|28|-|61|cm|abbr=on}}. The "moderate" scenario, where {{CO2}} ''emissions'' take a decade or two to peak and its atmospheric ''concentration'' does not plateau until the 2070s is called RCP 4.5. Its likely range of sea level rise is {{cvt|36–71|cm|in|frac=2}}. The highest scenario in RCP8.5 pathway sea level would rise between {{cvt|52 and 98|cm|in|frac=2}}.<ref name="ipcc13" /><ref name="CAT" >{{cite web |url=https://climateactiontracker.org/global/cat-thermometer/ |title=The CAT Thermometer |access-date=8 January 2023}}</ref> AR6 had equivalents for both scenarios, but it estimated larger sea level rise under both. In AR6, the SSP1-2.6 pathway results in a range of {{cvt|32–62|cm|in|frac=2}} by 2100. The "moderate" SSP2-4.5 results in a {{cvt|44–76|cm|in|frac=2}} range by 2100 and SSP5-8.5 led to {{cvt|65–101|cm|in|frac=2}}.<ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1302}}

This general increase of projections in AR6 came after the improvements in ice-sheet modelling and the incorporation of structured expert judgements.<ref name="Kopp2023" /> These decisions came as the observed ice-sheet erosion [[Climate change in the Arctic|in Greenland]] and [[Climate change in Antarctica|Antarctica]] had matched the upper-end range of the AR5 projections by 2020,<ref>{{cite news |title=Ice sheet melt on track with 'worst-case climate scenario' |language=en |work=www.esa.int |url=https://www.esa.int/Applications/Observing_the_Earth/Space_for_our_climate/Ice_sheet_melt_on_track_with_worst-case_climate_scenario |access-date=8 September 2020}}</ref><ref name="Slater-2020">{{cite journal |last1=Slater |first1=Thomas |last2=Hogg |first2=Anna E. |last3=Mottram |first3=Ruth |author-link3=Ruth Mottram |date=31 August 2020 |title=Ice-sheet losses track high-end sea-level rise projections |url=https://www.nature.com/articles/s41558-020-0893-y |journal=Nature Climate Change |language=en |volume=10 |issue=10 |pages=879–881 |bibcode=2020NatCC..10..879S |doi=10.1038/s41558-020-0893-y |issn=1758-6798 |archive-url=https://web.archive.org/web/20200902132539/https://www.nature.com/articles/s41558-020-0893-y |archive-date=2 September 2020 |access-date=8 September 2020 |s2cid=221381924}}</ref> and the finding that AR5 projections were likely too slow next to an extrapolation of observed sea level rise trends, while the subsequent reports had improved in this regard.<ref name="Grinsted-2021">{{Cite journal |last1=Grinsted |first1=Aslak |last2=Christensen |first2=Jens Hesselbjerg |date=2 February 2021 |title=The transient sensitivity of sea level rise |url=https://os.copernicus.org/articles/17/181/2021/ |journal=Ocean Science |volume=17 |issue=1 |pages=181–186 |bibcode=2021OcSci..17..181G |doi=10.5194/os-17-181-2021 |issn=1812-0784 |s2cid=234353584 |doi-access=free}}</ref> Further, AR5 was criticized by multiple researchers for excluding detailed estimates the impact of "low-confidence" processes like marine ice sheet and marine ice cliff instability,<ref name="pmid30013142" /><ref name="Pollard2015" /><ref name="Hansen2016">{{cite journal |last1=Hansen |first1=James |last2=Sato |first2=Makiko |last3=Hearty |first3=Paul |last4=Ruedy |first4=Reto |last5=Kelley |first5=Maxwell |last6=Masson-Delmotte |first6=Valerie |last7=Russell |first7=Gary |last8=Tselioudis |first8=George |last9=Cao |first9=Junji |last10=Rignot |first10=Eric |last11=Velicogna |first11=Isabella |date=22 March 2016 |title=Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming could be dangerous |journal=Atmospheric Chemistry and Physics |volume=16 |issue=6 |pages=3761–3812 |arxiv=1602.01393 |bibcode=2016ACP....16.3761H |doi=10.5194/acp-16-3761-2016 |first18=Michael |first19=Kwok-Wai |last19=Lo |first12=Blair |last18=Bauer |first17=Allegra N. |last17=Legrande |first16=Pushker |last16=Kharecha |first15=Karina |last15=von Schuckmann |first14=Evgeniya |last14=Kandiano |first13=Bailey |last13=Donovan |last12=Tormey |author-link11=Isabella Velicogna |s2cid=9410444 |doi-access=free}}</ref> which can substantially accelerate ice loss to potentially add "tens of centimeters" to sea level rise within this century.<ref name="ipcc13" /> AR6 includes a version of SSP5-8.5 where these processes take place, and in that case, sea level rise of up to {{cvt|1.6|m|ft|frac=3}} by 2100 could not be ruled out.<ref name="IPCC AR6 WG1 Ch.9">{{Cite journal |last1=Fox-Kemper |first1=B. |last2=Hewitt |first2=Helene T. |author2-link=Helene Hewitt |last3=Xiao |first3=C. |last4=Aðalgeirsdóttir |first4=G. |last5=Drijfhout |first5=S. S. |last6=Edwards |first6=T. L. |last7=Golledge |first7=N. R. |last8=Hemer |first8=M. |last9=Kopp |first9=R. E. |last10=Krinner |first10=G. |last11=Mix |first11=A. |date=2021 |editor-last=Masson-Delmotte |editor-first=V. |editor2-last=Zhai |editor2-first=P. |editor3-last=Pirani |editor3-first=A. |editor4-last=Connors |editor4-first=S. L. |editor5-last=Péan |editor5-first=C. |editor6-last=Berger |editor6-first=S. |editor7-last=Caud |editor7-first=N. |editor8-last=Chen |editor8-first=Y. |editor9-last=Goldfarb |editor9-first=L. |title=Chapter 9: Ocean, Cryosphere and Sea Level Change |url=https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_Chapter09.pdf |journal=Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change |publisher=Cambridge University Press, Cambridge, UK and New York, New York, US |page=}}</ref>{{Rp|page=1302}}

==== Role of instability processes ====
[[File:Zhang 2022 MISI and MICI.png|thumb|The stages of marine ice sheet (top) and marine ice cliff (bottom) instabilities. Dashed lines show that the retreat would be much more rapid if ice cliff instability were applicable <ref name="Zhang2022" />]]
The greatest uncertainty with sea level rise projections is associated with the so-called [[marine ice sheet instability]] (MISI), and, even more so, ''Marine Ice Cliff Instability'' (MICI).<ref name="Robel2019" /><ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1302}} These processes are mainly associated with West Antarctic Ice Sheet, but may also apply to some of Greenland's glaciers.<ref name="Zhang2022" /> The former suggests that when glaciers are mostly underwater on retrograde (backwards-sloping) bedrock, the water melts more and more of their height as their retreat continues, thus accelerating their breakdown on its own. This is widely accepted, but is difficult to model.<ref name="Robel2019" /><ref name="Zhang2022" />

The latter posits that coastal ice cliffs which exceed ~{{cvt|90|m|ft|frac=2}} in above-ground height and are ~{{cvt|800|m|ft|frac=2}} in basal (underground) height are likely to rapidly collapse under their own weight once the [[ice shelf|ice shelves]] propping them up are gone.<ref name="Zhang2022" /> The collapse then exposes the ice masses following them to the same instability, potentially resulting in a self-sustaining cycle of cliff collapse and rapid ice sheet retreat.<ref name="Pollard2015" /><ref name="Pattyn 2018">{{Cite journal |last=Pattyn |first=Frank |author-link=Frank Pattyn |date=2018 |title=The paradigm shift in Antarctic ice sheet modelling |journal=Nature Communications |language=En |volume=9 |issue=1 |page=2728 |bibcode=2018NatCo...9.2728P |doi=10.1038/s41467-018-05003-z |issn=2041-1723 |pmc=6048022 |pmid=30013142}}</ref><ref>{{Cite journal|last1=Dow|first1=Christine F.|last2=Lee|first2=Won Sang|last3=Greenbaum|first3=Jamin S.|last4=Greene|first4=Chad A.|last5=Blankenship|first5=Donald D.|last6=Poinar|first6=Kristin|last7=Forrest|first7=Alexander L.|last8=Young|first8=Duncan A.|last9=Zappa|first9=Christopher J.|date=2018-06-01|title=Basal channels drive active surface hydrology and transverse ice shelf fracture|journal=Science Advances|language=en|volume=4|issue=6|pages=eaao7212|doi=10.1126/sciadv.aao7212|issn=2375-2548|pmc=6007161|pmid=29928691|bibcode=2018SciA....4.7212D}}</ref> This theory had been highly influential - in a 2020 survey of 106 experts, the 2016 paper which suggested {{cvt|1|m|ft|frac=2}} or more of sea level rise by 2100 from Antarctica alone,<ref name="DeConto2016"/> was considered even more important than the 2014 [[IPCC Fifth Assessment Report]].<ref name="Horton2020">{{Cite journal |last1=Horton |first1=Benjamin P. |last2=Khan |first2=Nicole S. |last3=Cahill |first3=Niamh |last4=Lee |first4=Janice S. H. |last5=Shaw |first5=Timothy A. |last6=Garner |first6=Andra J. |last7=Kemp |first7=Andrew C. |last8=Engelhart |first8=Simon E. |last9=Rahmstorf |first9=Stefan |date=2020-05-08 |title=Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey |journal=npj Climate and Atmospheric Science |volume=3 |issue=1 |page=18 |doi=10.1038/s41612-020-0121-5 |bibcode=2020npjCA...3...18H |s2cid=218541055 |hdl=10356/143900 |hdl-access=free}}</ref> Even more rapid sea level rise was proposed in a 2016 study led by [[Jim Hansen]], which hypothesized multi-meter sea level rise in 50-100 years as a plausible outcome of high emissions,<ref name="Hansen2016" /> but it remains a minority view amongst the scientific community.<ref>{{cite news |year=2015 |title=James Hansen's controversial sea level rise paper has now been published online |newspaper=The Washington Post |url=https://www.washingtonpost.com/news/energy-environment/wp/2015/07/23/controversial-sea-level-rise-paper-is-now-published-online/ |quote="There is no doubt that the sea level rise, within the IPCC, is a very conservative number," says [[Greg Holland]], a climate and hurricane researcher at the [[National Center for Atmospheric Research]], who has also reviewed the Hansen study. "So the truth lies somewhere between IPCC and Jim."}}</ref>
[[File:Schlemm 2022 MICI embayment.png|thumb|left|If MICI can occur, the structure of the glacier [[embayment]] (viewed from the top) would do a lot to determine how quickly it may proceed<ref name="Schlemm2022" />]]
Marine ice cliff instability had also been very controversial, since it was proposed as a modelling exercise,<ref name="Zhang2022">{{Cite conference |last=Zhang |first=Zhe |date=7 November 2021 |title=Reviewing the elements of marine ice cliff instability |conference=The International Conference on Materials Chemistry and Environmental Engineering (CONF-MCEE 2021) |location=California, United States |url=https://iopscience.iop.org/article/10.1088/1742-6596/2152/1/012057/pdf |journal=Journal of Physics: Conference Series |volume=2152 |doi=10.1088/1742-6596/2152/1/012057}}</ref> and the observational evidence from both the past and the present is very limited and ambiguous.<ref name="Gilford2020" /> So far, only one episode of [[seabed gouging by ice]] from the [[Younger Dryas]] period appears truly consistent with this theory,<ref name="Wise2017" /> but it had lasted for an estimated 900 years,<ref name="Wise2017">{{Cite journal |last1=Wise |first1=Matthew G. |last2=Dowdeswell |first2=Julian A. |last3=Jakobsson |first3=Martin |last4=Larter |first4=Robert D. |date=October 2017 |title=Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks |url=https://nora.nerc.ac.uk/id/eprint/514800/1/Nature_final_accepted_ms.pdf |journal=Nature |language=en |volume=550 |issue=7677 |pages=506–510 |doi=10.1038/nature24458 |pmid=29072274 |bibcode=2017Natur.550..506W |issn=0028-0836 |archive-url=https://web.archive.org/web/20200506155034/https://nora.nerc.ac.uk/id/eprint/514800/1/Nature_final_accepted_ms.pdf |archive-date=May 6, 2020}}</ref> so it is unclear if it supports rapid sea level rise in the present.<ref name="Gilford2020" /> Modelling which investigated the hypothesis after 2016 often suggested that the ice shelves in the real world may collapse too slowly to make this scenario relevant,<ref>{{cite journal |last1=Clerc |first1=Fiona |last2=Minchew |first2=Brent M. |last3=Behn |first3=Mark D. |date=21 October 2019 |title=Marine Ice Cliff Instability Mitigated by Slow Removal of Ice Shelves |url=https://agupubs.onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2019GL084183 |journal=Geophysical Research Letters |volume=50 |issue=4 |pages=e2022GL102400 |doi=10.1029/2019GL084183 |via=American Geophysical Union}}</ref> or that [[ice mélange]] - debris produced as the glacier breaks down - would quickly build up in front of the glacier and significantly slow or even outright stop the instability soon after it began.<ref>{{cite news|url=https://www.sciencenews.org/article/climate-marine-ice-cliffs-sheets-collapse-not-inevitable-sea-level|title=Collapse may not always be inevitable for marine ice cliffs|last1=Perkins|first1=Sid|date=17 June 2021|access-date=9 January 2023|agency=ScienceNews}}</ref><ref>{{Cite journal |last1=Bassis |first1=J. N. |last2=Berg |first2=B. |last3=Crawford |first3=A. J. |last4=Benn |first4=D. I. |date=18 June 2021 |title=Transition to marine ice cliff instability controlled by ice thickness gradients and velocity |url=https://www.science.org/doi/10.1126/science.abf6271 |journal=Science |language=en |volume=372 |issue=6548 |pages=1342–1344 |bibcode=2021Sci...372.1342B |doi=10.1126/science.abf6271 |issn=0036-8075 |pmid=34140387 |hdl-access=free |hdl=10023/23422}}</ref><ref>{{Cite journal |last1=Crawford |first1=Anna J. |last2=Benn |first2=Douglas I. |last3=Todd |first3=Joe |last4=Åström |first4=Jan A. |last5=Bassis |first5=Jeremy N. |last6=Zwinger |first6=Thomas |date=11 May 2021 |title=Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization |url=https://www.nature.com/articles/s41467-021-23070-7 |journal=Nature Communications |volume=12 |doi=10.1038/s41467-021-23070-7}}</ref><ref name="Schlemm2022">{{Cite journal |last1=Schlemm |first1=Tanja |last2=Feldmann |first2=Johannes |last3=Winkelmann |first3=Ricarda |last4=Levermann |first4=Anders |date=24 May 2022 |title=Stabilizing effect of mélange buttressing on the marine ice-cliff instability of the West Antarctic Ice Sheet |journal=The Cryosphere |volume=16 |issue=5 |pages=1979–1996 |doi=10.5194/tc-16-1979-2022 |doi-access=free}}</ref>

Due to these uncertainties, some scientists - including the originators of the hypothesis, Robert DeConto and David Pollard - have suggested that the best way to resolve the question would be to precisely determine sea level rise during the [[Last Interglacial]].<ref name="Gilford2020" /> MICI can be effectively ruled out if SLR at the time was lower than {{cvt|4|m|ft|frac=2}}, while it is very likely if the SLR was greater than {{cvt|6|m|ft|frac=2}}.<ref name="Gilford2020">{{cite journal |last1=Gilford |first1=Daniel M. |last2=Ashe |first2=Erica L. |last3=DeConto |first3=Robert M. |last4=Kopp |first4=Robert E. |last5=Pollard |first5=David |last6=Rovere |first6=Alessio |date=5 October 2020 |title=Could the Last Interglacial Constrain Projections of Future Antarctic Ice Mass Loss and Sea-Level Rise? |url=https://agupubs.onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2019JF005418 |journal=Journal of Geophysical Research: Earth Surface |volume=124 |issue=7 |pages=1899-1918 |doi=10.1029/2019JF005418 |via=American Geophysical Union}}</ref> As of 2023, the most recent analysis indicates that the Last Interglacial SLR is unlikely to have been higher than {{cvt|2.7|m|ft|frac=2}},<ref name="Dumitru2023" /> as higher values in other research, such as {{cvt|5.7|m|ft|frac=2}},<ref>{{cite journal |last1=Barnett |first1=Robert L. |last2=Austermann |first2=Jacqueline |last3=Dyer |first3=Blake |last4=Telfer |first4=Matt W. |last5=Barlow |first5=Natasha L. M. |last6=Boulton |first6=Sarah J. |last7=Carr |first7=Andrew S. |last8=Creel |first8=Roger |date=15 September 2023 |title=Constraining the contribution of the Antarctic Ice Sheet to Last Interglacial sea level |url=https://www.science.org/doi/10.1126/sciadv.adf0198 |journal=Science Advances |volume=9 |issue=27 |doi=10.1126/sciadv.adf0198}}</ref> appear inconsistent with the new [[paleoclimate]] data from [[The Bahamas]] and the known history of the Greenland Ice Sheet.<ref name="Dumitru2023">{{cite journal |last1=Dumitru |first1=Oana A. |last2=Dyer |first2=Blake |last3=Austermann |first3=Jacqueline |last4=Sandstrom |first4=Michael R. |last5=Goldstein |first5=Steven L. |last6=D'Andrea |first6=William J. |last7=Cashman |first7=Miranda |last8=Creel |first8=Roger |last9=Bolge |first9=Louise |last10=Raymo |first10=Maureen E. |date=15 September 2023 |title=Last interglacial global mean sea level from high-precision U-series ages of Bahamian fossil coral reefs |url=https://www.sciencedirect.com/science/article/pii/S0277379123003359 |journal=Quaternary Science Reviews |volume=318 |page=108287 |doi=10.1016/j.quascirev.2023.108287}}</ref>

=== Post-2100 sea level rise ===
[[File:1900-2300 Long-term projections of sea level rise.svg|thumb|upright=1.35|If countries cut greenhouse gas emissions significantly (lowest trace), sea level rise by 2100 will be limited to 0.3 to 0.6 meters (1–2 feet).<ref name=NASA_SLR_2021/> However, in a worst-case scenario (top trace), sea levels could rise 5 meters (16 feet) by the year 2300.<ref name=NASA_SLR_2021>{{cite web |title=Anticipating Future Sea Levels |url=https://earthobservatory.nasa.gov/images/148494/anticipating-future-sea-levels |website=EarthObservatory.NASA.gov |publisher=National Aeronautics and Space Administration (NASA) |archive-url=https://web.archive.org/web/20210707220354/https://earthobservatory.nasa.gov/images/148494/anticipating-future-sea-levels |archive-date=7 July 2021 |date=2021 |url-status=live}}</ref>]]
Even if the temperature stabilizes, significant sea-level rise (SLR) will continue for centuries,<ref name="nrccon">{{cite book |author=National Research Council |title=Advancing the Science of Climate Change |publisher=The National Academies Press |year=2010 |isbn=978-0-309-14588-6 |location=Washington, DC |page=245 |chapter=7 Sea Level Rise and the Coastal Environment |doi=10.17226/12782 |access-date=2011-06-17 |chapter-url=http://books.nap.edu/openbook.php?record_id=12782&page=245}}</ref> consistent with [[proxy (climate)|paleo records]] of sea level rise.<ref name="ipcc13" />{{rp|1189}} This is due to the high level of inertia in the carbon cycle and the climate system, owing to factors such as the slow diffusion of heat into the [[Ocean temperature#Deep ocean temperature|deep ocean]], leading to a longer climate response time.<ref>{{Cite journal |last1=Hansen |first1=J. |last2=Russell |first2=G. |last3=Lacis |first3=A. |last4=Fung |first4=I. |last5=Rind |first5=D. |last6=Stone |first6=P. |date=1985-08-30 |title=Climate Response Times: Dependence on Climate Sensitivity and Ocean Mixing |url=https://pubs.giss.nasa.gov/docs/1985/1985_Hansen_ha09600g.pdf |journal=Science |language=en |volume=229 |issue=4716 |pages=857–859 |doi=10.1126/science.229.4716.857 |pmid=17777925 |bibcode=1985Sci...229..857H |issn=0036-8075 |archive-url=https://web.archive.org/web/20210327184018/https://pubs.giss.nasa.gov/docs/1985/1985_Hansen_ha09600g.pdf |archive-date=March 27, 2021 |via=NASA}}</ref> A 2018 paper estimated that sea level rise in 2300 would increase by a median of 20&nbsp;cm (8&nbsp;in) for every five years {{CO2}} emissions increase before peaking. It shows a 5% likelihood of a {{cvt|1|m|ft|frac=2}} increase due to the same. The same estimate found that if the temperature stabilized below {{convert|2|C-change|F-change}}, 2300 sea level rise would still exceed {{cvt|1.5|m|ft|frac=2}}. Early [[net zero]] and slowly falling temperatures could limit it to {{cvt|70–120|cm|in|frac=2}}.<ref>{{Cite journal |last1=Mengel |first1=Matthias |last2=Nauels |first2=Alexander |last3=Rogelj |first3=Joeri |last4=Schleussner |first4=Carl-Friedrich |date=20 February 2018 |title=Committed sea-level rise under the Paris Agreement and the legacy of delayed mitigation action |journal=Nature Communications |volume=9 |issue=1 |page=601 |doi=10.1038/s41467-018-02985-8 |pmid=29463787 |pmc=5820313 |bibcode=2018NatCo...9..601M}}</ref>

By 2021, the [[IPCC Sixth Assessment Report]] was able to provide estimates for sea level rise in 2150. Keeping warming to 1.5{{Nbsp}}°C under the SSP1-1.9 scenario would result in sea level rise in the 17–83% range of {{cvt|37–86|cm|in|frac=2}}. In the SSP1-2.6 pathway the range would be {{cvt|46–99|cm|in|frac=2}}, for SSP2-4.5 a {{cvt|66–133|cm|in|frac=2}} range by 2100 and for SSP5-8.5 a rise of {{cvt|98–188|cm|in|frac=2}}. It stated that the "low-confidence, high impact" projected {{cvt|0.63-1.60|m|ft|frac=2}} mean sea level rise by 2100, and that by 2150, the total sea level rise in his scenario would be in the range of {{cvt|0.98 - 4.82|m|ft|frac=2}} by 2150.<ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1302}} AR6 also provided lower-confidence estimates for year 2300 sea level rise under SSP1-2.6 and SSP5-8.5 with various impact assumptions. In the best case scenario, under SSP1-2.6 with no ice sheet acceleration after 2100, the estimate was only {{Convert|0.8 - 2.0|m|ft}}. In the worst estimated scenario, SSP-8.5 with ice cliff instability, the projected range for total sea level rise was {{Convert|9.5 - 16.2|m|ft}} by the year 2300.<ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1306}}

Projections for subsequent years are more difficult. In 2019, when 22 experts on ice sheets were asked to estimate 2200 and 2300 SLR under the 5{{Nbsp}}°C warming scenario, there were 90% [[confidence interval]]s of −{{cvt|10|cm|in|frac=2}} to {{cvt|740|cm|ft|frac=2}} and −{{cvt|9|cm|in|frac=2}} to {{cvt|970|cm|ft|frac=2}}, respectively. (Negative values represent the extremely low probability of large climate change-induced increases in [[precipitation]] greatly elevating ice sheet [[surface mass balance]].)<ref name="PNAS22">{{cite journal |last1=Bamber |first1=Jonathan L. |last2=Oppenheimer |first2=Michael |last3=Kopp |first3=Robert E. |last4=Aspinall |first4=Willy P. |last5=Cooke |first5=Roger M. |date=May 2019 |title=Ice sheet contributions to future sea-level rise from structured expert judgment |journal=Proceedings of the National Academy of Sciences |volume=116 |issue=23 |pages=11195–11200 |bibcode=2019PNAS..11611195B |doi=10.1073/pnas.1817205116 |pmc=6561295 |pmid=31110015 |doi-access=free}}</ref> In 2020, 106 experts who contributed to 6 or more papers on sea level estimated median {{cvt|118|cm|in|frac=2}} SLR in the year 2300 for the low-warming RCP2.6 scenario and the median of {{cvt|329|cm|in|frac=2}} for the high-warming RCP8.5. The former scenario had the 5%–95% confidence range of {{cvt|24–311|cm|in|frac=2}}, and the latter of {{cvt|88–783|cm|in|frac=2}}.<ref name="Horton2020" />

[[File:6m Sea Level Rise.jpg|thumb|upright=1.35|Map of the Earth with a long-term {{Convert|6|m|ft|adj=on}} sea level rise represented in red (uniform distribution, actual sea level rise will vary regionally and [[#Adaptation|local adaptation measures]] will also have an effect on local sea levels).|alt=A map showing major SLR impact in south-east Asia, Northern Europe and the East Coast of the US]]

After 500 years, sea level rise from thermal expansion alone may have reached only half of its eventual level - likely within ranges of {{cvt|0.5-2|m|ft|frac=2}}.<ref name="solomon">{{cite journal |last1=Solomon |first1=Susan |last2=Plattner |first2=Gian-Kasper |last3=Knutti |first3=Reto |last4=Friedlingstein |first4=Pierre |date=10 February 2009 |title=Irreversible climate change due to carbon dioxide emissions |journal=Proceedings of the National Academy of Sciences |volume=106 |issue=6 |pages=1704–1709 |bibcode=2009PNAS..106.1704S |doi=10.1073/pnas.0812721106 |pmc=2632717 |pmid=19179281 |doi-access=free}}</ref> Additionally, [[tipping points in the climate system|tipping points]] of Greenland and Antarctica ice sheets are likely to play a larger role over such timescales.<ref name="Pattyn-2018">{{cite journal |last1=Pattyn |first1=Frank |last2=Ritz |first2=Catherine |last3=Hanna |first3=Edward |last4=Asay-Davis |first4=Xylar |last5=DeConto |first5=Rob |last6=Durand |first6=Gaël |last7=Favier |first7=Lionel |last8=Fettweis |first8=Xavier |last9=Goelzer |first9=Heiko |last10=Golledge |first10=Nicholas R. |last11=Kuipers Munneke |first11=Peter |date=12 November 2018 |title=The Greenland and Antarctic ice sheets under 1.5 °C global warming |url=https://dipot.ulb.ac.be/dspace/bitstream/2013/278021/3/ReviewOnePointFive_v7.pdf |journal=Nature Climate Change |volume=8 |issue=12 |pages=1053–1061 |bibcode=2018NatCC...8.1053P |doi=10.1038/s41558-018-0305-8 |first13=Sophie |last13=Nowicki |s2cid=91886763 |last12=Lenaerts |first18=Michiel |last14=Payne |last18=van den Broeke |first17=Luke D. |last17=Trusel |first16=Hélène |last16=Seroussi |first15=Alexander |last15=Robinson |first14=Antony J. |first12=Jan T. M.}}</ref> Ice loss from [[Antarctica]] is likely to dominate very long-term SLR, especially if the warming exceeds {{convert|2|C-change|F-change}}. Continued carbon dioxide emissions from fossil fuel sources could cause additional tens of metres of sea level rise, over the next millennia.<ref>{{Cite journal |last1=Clark |first1=Peter U. |last2=Shakun |first2=Jeremy D. |last3=Marcott |first3=Shaun A. |last4=Mix |first4=Alan C. |last5=Eby |first5=Michael |date=April 2016 |title=Consequences of twenty-first-century policy for multi-millennial climate and sea-level change |url=https://ir.library.oregonstate.edu/concern/articles/mk61rj62n |journal=Nature Climate Change |language=en |volume=6 |issue=4 |pages=360–369 |doi=10.1038/nclimate2923 |bibcode=2016NatCC...6..360C |issn=1758-6798 |archive-url=https://web.archive.org/web/20200711054610/https://ir.library.oregonstate.edu/downloads/5999n523k |archive-date=July 11, 2020 |via=Oregon State University}}</ref> Burning of all fossil fuels on Earth is sufficient to melt the entire Antarctic ice sheet, causing about {{Cvt|58|m|ft}} of sea level rise.<ref>{{cite journal |last1=Winkelmann |first1=Ricarda |author1-link=Ricarda Winkelmann |last2=Levermann |first2=Anders |last3=Ridgwell |first3=Andy |last4=Caldeira |first4=Ken |date=11 September 2015 |title=Combustion of available fossil fuel resources sufficient to eliminate the Antarctic Ice Sheet |journal=Science Advances |volume=1 |issue=8 |pages=e1500589 |bibcode=2015SciA....1E0589W |doi=10.1126/sciadv.1500589 |pmc=4643791 |pmid=26601273}}</ref>

Year 2021 IPCC estimates for the amount of sea level rise over the next 2,000 years project that:

* At a warming peak of {{convert|1.5|C-change|F-change}}, global sea levels would rise {{cvt|2-3|m|ft|frac=2}}
* At a warming peak of {{convert|2|C-change|F-change}}, sea levels would rise {{cvt|2-6|m|ft|frac=2}}
* At a warming peak of {{convert|5|C-change|F-change}}, sea levels would rise {{cvt|19-22|m|ft|frac=2}}<ref name="IPCC_2021_WGI_SPM" />{{rp|SPM-21}}

Sea levels would continue to rise for several thousand years after the ceasing of emissions, due to the slow nature of climate response to heat. The same estimates on a timescale of 10,000 years project that:

* At a warming peak of {{convert|1.5|C-change|F-change}}, global sea levels would rise {{cvt|6-7|m|ft|frac=2}}
* At a warming peak of {{convert|2|C-change|F-change}}, sea levels would rise {{cvt|8-13|m|ft|frac=2}} 
* At a warming peak of {{convert|5|C-change|F-change}}, sea levels would rise {{cvt|28-37|m|ft|frac=2}}<ref name="IPCC AR6 WG1 Ch.9" />{{rp|1306}}

== Measurements ==
Variations in the amount of water in the oceans, changes in its volume, or varying land elevation compared to the sea surface can drive sea level changes. Over a consistent time period, assessments can attribute contributions to sea level rise and provide early indications of change in trajectory. This helps to inform adaptation plans.<ref>{{Cite web |title=2022 Sea Level Rise Technical Report |url=https://oceanservice.noaa.gov/hazards/sealevelrise/sealevelrise-tech-report.html#step4 |access-date=2022-02-22 |website=oceanservice.noaa.gov |language=EN-US}}</ref> The different techniques used to measure changes in sea level do not measure exactly the same level. Tide gauges can only measure relative sea level. [[Satellite]]s can also measure absolute sea level changes.<ref name="Rovere-2016-2">{{cite journal |last1=Rovere |first1=Alessio |last2=Stocchi |first2=Paolo |last3=Vacchi |first3=Matteo |date=2 August 2016 |title=Eustatic and Relative Sea Level Changes |journal=Current Climate Change Reports |volume=2 |issue=4 |pages=221–231 |doi=10.1007/s40641-016-0045-7 |bibcode=2016CCCR....2..221R |s2cid=131866367 |doi-access=free}}</ref> To get precise measurements for sea level, researchers studying the ice and oceans factor in ongoing [[Geomorphology|deformations of the solid Earth]]. They look in particular at [[Glacial isostatic adjustment|landmasses still rising from past ice masses retreating]], and the [[Gravity of Earth|Earth's gravity]] and [[Earth's rotation|rotation]].<ref name="WCRP2018" />

===Satellites===
[[File:TOPEX-JasonSeries2008.jpg|left|thumb|upright=1.4|[[Jason-1]] continued the sea surface measurements started by TOPEX/Poseidon. It was followed by the [[Ocean Surface Topography Mission]] on [[Jason-2]], and by [[Jason-3]].]]
Since the launch of [[TOPEX/Poseidon]] in 1992, an overlapping series of [[Satellite geodesy#Altimetry|altimetric satellites]] has been continuously recording the sea level and its changes.<ref>{{cite web |title=Ocean Surface Topography from Space |url=http://sealevel.jpl.nasa.gov/missions/topex/ |archive-url=https://web.archive.org/web/20110722010847/http://sealevel.jpl.nasa.gov/missions/topex/ |archive-date=2011-07-22 |publisher=NASA/JPL}}</ref> These satellites can measure the hills and valleys in the sea caused by currents and detect trends in their height. To measure the distance to the sea surface, the satellites send a microwave pulse towards Earth and record the time it takes to return after reflecting off the ocean's surface. [[Microwave radiometer]]s correct the additional delay caused by [[water vapor]] in the [[atmosphere]]. Combining these data with the location of the spacecraft determines the sea-surface height to within a few centimetres.<ref>{{Cite web |title=Jason-3 Satellite – Mission |url=https://www.nesdis.noaa.gov/jason-3/mission.html |access-date=2018-08-22 |website=www.nesdis.noaa.gov}}</ref> These satellite measurements have estimated rates of sea level rise for 1993–2017 at {{convert|3.0|±|0.4|mm|frac=64|in}} per year.<ref name="Nerem-2018">{{cite journal |last1=Nerem |first1=R. S. |last2=Beckley |first2=B. D. |last3=Fasullo |first3=J. T. |last4=Hamlington |first4=B. D. |last5=Masters |first5=D. |last6=Mitchum |first6=G. T. |date=27 February 2018 |title=Climate-change–driven accelerated sea-level rise detected in the altimeter era |journal=Proceedings of the National Academy of Sciences of the United States of America |volume=115 |issue=9 |pages=2022–2025 |bibcode=2018PNAS..115.2022N |doi=10.1073/pnas.1717312115 |pmc=5834701 |pmid=29440401 |doi-access=free}}</ref>

Satellites are useful for measuring regional variations in sea level. An example is the substantial rise between 1993 and 2012 in the western tropical Pacific. This sharp rise has been linked to increasing [[trade winds]]. These occur when the [[Pacific Decadal Oscillation]] (PDO) and the [[El Niño–Southern Oscillation]] (ENSO) change from one state to the other.<ref>{{cite journal |last1=Merrifield |first1=Mark A. |last2=Thompson |first2=Philip R. |last3=Lander |first3=Mark |date=July 2012 |title=Multidecadal sea level anomalies and trends in the western tropical Pacific |journal=Geophysical Research Letters |volume=39 |issue=13 |pages=n/a |bibcode=2012GeoRL..3913602M |doi=10.1029/2012gl052032 |s2cid=128907116}}</ref> The PDO is a basin-wide climate pattern consisting of two phases, each commonly lasting 10 to 30 years. The ENSO has a shorter period of 2 to 7 years.<ref>{{cite journal |last1=Mantua |first1=Nathan J. |last2=Hare |first2=Steven R. |last3=Zhang |first3=Yuan |last4=Wallace |first4=John M. |last5=Francis |first5=Robert C. |date=June 1997 |title=A Pacific Interdecadal Climate Oscillation with Impacts on Salmon Production |journal=Bulletin of the American Meteorological Society |volume=78 |issue=6 |pages=1069–1079 |bibcode=1997BAMS...78.1069M |doi=10.1175/1520-0477(1997)078<1069:APICOW>2.0.CO;2 |doi-access=free}}</ref>

=== Tide gauges ===
[[File:Sea_level_change_1993_to_2018.jpg|thumb|upright=1.4|Between 1993 and 2018, the mean sea level has risen across most of the world ocean (blue colors).<ref>Lindsey, Rebecca (2019) [https://www.climate.gov/news-features/understanding-climate/climate-change-global-sea-level Climate Change: Global Sea Level] ''NOAA Climate'', 19 November 2019.</ref>]]
The global network of [[tide gauge]]s is the other important source of sea-level observations. Compared to the satellite record, this record has major spatial gaps but covers a much longer period.<ref name="Rhein-2013">{{Cite book |last1=Rhein |first1=Monika |title=IPCC AR5 WGI |last2=Rintoul |first2=Stephan |publisher=Cambridge University Press |year=2013 |location=New York |page=285 |chapter=Observations: Ocean |author-link1=Monika Rhein |access-date=2018-08-26 |chapter-url=https://ipcc.ch/pdf/assessment-report/ar5/wg1/WG1AR5_Chapter03_FINAL.pdf |archive-url=https://web.archive.org/web/20180613012554/https://www.ipcc.ch/pdf/assessment-report/ar5/wg1/WG1AR5_Chapter03_FINAL.pdf |archive-date=2018-06-13}}</ref> Coverage of tide gauges started mainly in the [[Northern Hemisphere]]. Data for the [[Southern Hemisphere]] remained scarce up to the 1970s.<ref name="Rhein-2013" /> The longest running sea-level measurements, NAP or [[Amsterdam Ordnance Datum]] were established in 1675, in [[Amsterdam]].<ref>{{cite web |title=Other Long Records not in the PSMSL Data Set |url=http://www.psmsl.org/data/longrecords/ |access-date=11 May 2015 |publisher=PSMSL}}</ref> Record collection is also extensive in [[Australia]]. They include measurements by [[Thomas Lempriere]], an amateur meteorologist, beginning in 1837. Lempriere established a sea-level benchmark on a small cliff on the [[Isle of the Dead (Tasmania)|Isle of the Dead]] near the [[Port Arthur, Tasmania|Port Arthur]] convict settlement in 1841.<ref>{{cite journal |last=Hunter |first=John |author2=R. Coleman |author3=D. Pugh |date=2003 |title=The Sea Level at Port Arthur, Tasmania, from 1841 to the Present |url=https://figshare.com/articles/journal_contribution/22846694 |journal=Geophysical Research Letters |volume=30 |issue=7 |page=1401 |bibcode=2003GeoRL..30.1401H |doi=10.1029/2002GL016813 |s2cid=55384210}}</ref>

Together with satellite data for the period after 1992, this network established that global mean sea level rose {{Convert|19.5|cm|in|abbr=on}} between 1870 and 2004 at an average rate of about 1.44&nbsp;mm/yr. (For the 20th century the average is 1.7&nbsp;mm/yr.)<ref name="church2">{{cite journal |author=Church, J.A. |author2=White, N.J. |date=2006 |title=20th century acceleration in global sea-level rise |journal=Geophysical Research Letters |volume=33 |issue=1 |pages=L01602 |bibcode=2006GeoRL..33.1602C |citeseerx=10.1.1.192.1792 |doi=10.1029/2005GL024826 |s2cid=129887186}}</ref> By 2018, data collected by Australia's [[Commonwealth Scientific and Industrial Research Organisation]] (CSIRO) had shown that the global mean sea level was rising by {{Convert|3.2|mm|in|abbr=on|frac=32}} per year. This was double the average 20th century rate.<ref>{{Cite web |title=Historical sea level changes: Last decades |url=http://www.cmar.csiro.au/sealevel/sl_hist_last_decades.html |access-date=2018-08-26 |website=www.cmar.csiro.au}}</ref><ref>{{cite web |last=Neil |first=White |title=Historical Sea Level Changes |url=http://www.cmar.csiro.au/sealevel/sl_hist_few_hundred.html |access-date=25 April 2013 |publisher=CSIRO}}</ref> The 2023 [[World Meteorological Organization]] report found further acceleration to 4.62&nbsp;mm/yr over the 2013–2022 period.<ref name=WMO_20230421/> These observations help to check and verify predictions from climate change simulations.

Regional differences are also visible in the tide gauge data. Some are caused by local sea level differences. Others are due to vertical land movements. In [[Europe]], only some land areas are rising while the others are sinking. Since 1970, most tidal stations have measured higher seas. However sea levels along the northern [[Baltic Sea]] have dropped due to [[post-glacial rebound]].<ref>{{cite web |date=18 November 2021 |title=Global and European sea level rise |url=https://www.eea.europa.eu/ims/global-and-european-sea-level-rise |website=European Environment Agency}}</ref>

===Past sea level rise===

{{Main|Past sea level|Sea level#Change|Marine transgression}}
[[File:Post-Glacial Sea Level.png|thumb|upright=1.5| Changes in sea levels since the end of the [[Last glacial period|last glacial episode]]]]An understanding of [[past sea level]] is an important guide to where current changes in sea level will end up. In the recent geological past, thermal expansion from increased temperatures and changes in land ice are the dominant reasons of sea level rise. The last time that the Earth was {{convert|2|C-change|F-change}} warmer than pre-industrial temperatures was 120,000 years ago. This was when warming due to [[Milankovitch cycles]] (changes in the amount of sunlight due to slow changes in the Earth's orbit) caused the [[Eemian]] [[interglacial]]. Sea levels during that warmer interglacial were at least {{Convert|5|m|ft|abbr=on|}} higher than now.<ref>{{Cite web |date=2019-08-30 |title=Scientists discover evidence for past high-level sea rise |url=https://phys.org/news/2019-08-scientists-evidence-high-level-sea.html |access-date=2019-09-07 |website=phys.org |language=en-us}}</ref> The Eemian warming was sustained over a period of thousands of years. The size of the rise in sea level implies a large contribution from the Antarctic and Greenland ice sheets.<ref name="ipcc13" />{{rp|1139}} Levels of atmospheric carbon dioxide of around 400 [[parts per million]] (similar to 2000s) had increased temperature by over {{convert|2-3|C-change|F-change}} around three million years ago. This temperature increase eventually melted one third of Antarctica's ice sheet, causing sea levels to rise 20 meters above the preindustrial levels.<ref>{{Cite web |title=Present CO2 levels caused 20-metre-sea-level rise in the past |url=https://www.nioz.nl/en/news/present-co2-levels-caused-20-metre-sea-level-rise-in-the-past |publisher=Royal Netherlands Institute for Sea Research}}</ref>

Since the [[Last Glacial Maximum]], about 20,000 years ago, sea level has risen by more than {{Convert|125|m|ft|-1}}. Rates vary from less than 1&nbsp;mm/year during the pre-industrial era to 40+ mm/year when major ice sheets over Canada and Eurasia melted. [[Meltwater pulse 1A|Meltwater pulses]] are periods of fast sea level rise caused by the rapid disintegration of these ice sheets. The rate of sea level rise started to slow down about 8,200 years before today. Sea level was almost constant for the last 2,500 years. The recent trend of rising sea level started at the end of the 19th or beginning of the 20th century.<ref>{{cite journal |last1=Lambeck |first1=Kurt |last2=Rouby |first2=Hélène |last3=Purcell |first3=Anthony |last4=Sun |first4=Yiying |last5=Sambridge |first5=Malcolm |date=28 October 2014 |title=Sea level and global ice volumes from the Last Glacial Maximum to the Holocene |journal=Proceedings of the National Academy of Sciences of the United States of America |volume=111 |issue=43 |pages=15296–15303 |bibcode=2014PNAS..11115296L |doi=10.1073/pnas.1411762111 |pmc=4217469 |pmid=25313072 |doi-access=free}}</ref>

== Causes ==
[[File:Kopp 2023 4 contributions.png|thumb|upright=1.35|The main contributors to sea level rise, and how much they are expected to add by the end of the century under the low-emission scenario ("SSP1-2.6") and the high-emission scenario ("SSP5-8.5"). The Antarctic ice sheet is the least certain contributor <ref name="Kopp2023">{{cite journal |last1=Kopp |first1=Robert E. |last2=Garner |first2=Gregory G. |last3=Hermans |first3=Tim H. J. |last4=Jha |first4=Shantenu |last5=Kumar |first5=Praveen |last6=Reedy |first6=Alexander |last7=Slangen |first7=Aimée B. A. |last8=Turilli |first8=Matteo |last9=Edwards |first9=Tamsin L. |last10=Gregory |first10=Jonathan M. |last11=Koubbe |first11=George |last12=Levermann |first12=Anders |last13=Merzky |first13=Andre |last14=Nowicki |first14=Sophie |last15=Palmer |first15=Matthew D. |last16=Smith |first16=Chris |title=The Framework for Assessing Changes To Sea-level (FACTS) v1.0: a platform for characterizing parametric and structural uncertainty in future global, relative, and extreme sea-level change |journal=The Cryosphere |date=21 December 2023 |volume=16 |issue=24 |pages=7461–7489 |doi=10.5194/gmd-16-7461-2023 |doi-access=free |bibcode=2023GMD....16.7461K}}</ref> ]]

The three main reasons warming causes global sea level to rise are [[Thermal expansion#Expansion in liquids|the expansion of oceans due to heating]], water inflow from melting ice sheets and water inflow from glaciers. Glacier retreat and ocean expansion have dominated sea level rise since the start of the 20th century.<ref name="Mengel2016" /> Some of the losses from glaciers are offset when [[precipitation]] falls as snow, accumulates and over time forms glacial ice. If precipitation, surface processes and ice loss at the edge [[Glacier mass balance|balance]] each other, sea level remains the same. Because of this precipitation began as water vapor evaporated from the ocean surface, [[effects of climate change on the water cycle]] can even increase ice build-up. However, this effect is not enough to fully offset ice losses, and sea level rise continues to accelerate.<ref name="AR6_WGII_Chapter9" /><ref name="IMBIE2018" /><ref name="Rignot2019" /><ref name="Zwally2021" />

The contributions of the two large ice sheets, in [[Greenland ice sheet|Greenland]] and [[Antarctic ice sheet|Antarctica]], are likely to increase in the 21st century.<ref name="Mengel2016">{{cite journal |last1=Mengel |first1=Matthias |last2=Levermann |first2=Anders |last3=Frieler |first3=Katja |last4=Robinson |first4=Alexander |last5=Marzeion |first5=Ben |last6=Winkelmann |first6=Ricarda |title=Future sea level rise constrained by observations and long-term commitment |journal=Proceedings of the National Academy of Sciences |date=8 March 2016 |volume=113 |issue=10 |pages=2597–2602 |doi=10.1073/pnas.1500515113 |pmc=4791025 |pmid=26903648 |bibcode=2016PNAS..113.2597M |doi-access=free}}</ref> They store most of the land ice (~99.5%) and have a sea-level equivalent (SLE) of {{Convert|7.4|m|ftin|abbr=on}} for Greenland and {{Convert|58.3|m|ftin|abbr=on}} for Antarctica.<ref name="WCRP2018"/> Thus, melting of all the ice on Earth would result in about {{Convert|70|m|ftin|abbr=on}} of sea level rise,<ref>{{cite web |title=How would sea level change if all glaciers melted? |url=https://www.usgs.gov/faqs/how-would-sea-level-change-if-all-glaciers-melted |website=United States Geological Survey |access-date=15 January 2024}}</ref> although this would require at least 10,000 years and up to {{convert|10|C-change|F-change}} of global warming.<ref name="ArmstrongMcKay2022" /><ref name="ArmstrongMcKayExplainer" />

=== Ocean heating ===
{{Main|Ocean heat content}}
[[File:1955- Ocean heat content - NOAA.svg |thumb|left |upright=1.2|There has been an increase in ocean heat content during recent decades as the oceans absorb most of the [[Earth's energy budget|excess heat]] created by human-induced [[Global Warming|global warming]].<ref name=NOAA_NASA_OHC_1957_>''Top 700 meters:'' {{cite web |last1=Lindsey |first1=Rebecca |last2=Dahlman |first2=Luann |title=Climate Change: Ocean Heat Content |url=https://www.climate.gov/news-features/understanding-climate/climate-change-ocean-heat-content |website=climate.gov |publisher=National Oceanic and Atmospheric Administration (NOAA) |archive-url=https://archive.today/20231029171303/https://www.climate.gov/news-features/understanding-climate/climate-change-ocean-heat-content |archive-date=29 October 2023 |date=6 September 2023 |url-status=live}} ● ''Top 2000 meters:'' {{cite web |title=Ocean Warming / Latest Measurement: December 2022 / 345 (± 2) zettajoules since 1955 |url=https://climate.nasa.gov/vital-signs/ocean-warming/ |website=NASA.gov |publisher=National Aeronautics and Space Administration |archive-url=https://web.archive.org/web/20231020033606/https://climate.nasa.gov/vital-signs/ocean-warming/ |archive-date=20 October 2023 |url-status=live}}</ref>]]
The oceans store more than 90% of the extra heat added to the climate system by [[Earth's energy imbalance]] and act as a buffer against its effects.<ref>{{Cite journal |last1=Cheng |first1=Lijing |last2=Foster |first2=Grant |last3=Hausfather |first3=Zeke |last4=Trenberth |first4=Kevin E. |last5=Abraham |first5=John |date=2022 |title=Improved Quantification of the Rate of Ocean Warming |journal=Journal of Climate |volume=35 |issue=14 |pages=4827–4840 |bibcode=2022JCli...35.4827C |doi=10.1175/JCLI-D-21-0895.1 |doi-access=free}}</ref> This means that the same amount of heat that would increase the average world ocean temperature by {{convert|0.01|C-change|F-change}} would increase atmospheric temperature by approximately {{convert|10|C-change|F-change}}.<ref>{{cite journal |author1=Levitus, S. |author2=Boyer, T. |author3=Antonov, J. |title=Warming of the world ocean: 1955–2003 |year=2005 |journal=Geophysical Research Letters |volume=32 |issue=2 |doi=10.1029/2004GL021592 |doi-access=free|bibcode=2005GeoRL..32.2604L}}</ref> So a small change in the mean temperature of the ocean represents a very large change in the total heat content of the climate system. Winds and currents move heat into deeper parts of the ocean. Some of it reaches depths of more than {{Convert|2000|m|ft|sigfig=2|abbr=on}}.<ref>{{Cite web|url=https://www.scientificamerican.com/article/deep-ocean-waters-are-trapping-vast-stores-of-heat/|title=Deep Ocean Waters Are Trapping Vast Stores of Heat|last=Upton|first=John|date=2016-01-19|website=Scientific American|access-date=2019-02-01}}</ref>

When the ocean gains heat, [[thermal expansion|the water expands]] and sea level rises. Warmer water and water under great pressure (due to depth) expand more than cooler water and water under less pressure.<ref name="ipcc13" />{{rp|1161}} Consequently, cold [[Arctic Ocean]] water will expand less than warm tropical water. Different climate models present slightly different patterns of ocean heating. So their projections do not agree fully on how much ocean heating contributes to sea level rise.<ref>{{Cite journal|last1=Kuhlbrodt|first1=T|last2=Gregory|first2=J.M.|date=2012|title=Ocean heat uptake and its consequences for the magnitude of sea level rise and climate change|journal=Geophysical Research Letters|volume=39|issue=18|pages=L18608|doi=10.1029/2012GL052952|bibcode=2012GeoRL..3918608K|s2cid=19120823|url=http://centaur.reading.ac.uk/28951/1/Kuhlbrodt_Gregory_GRL_2012.pdf}}</ref>

=== Antarctic ice loss ===
[[File:Antarctic shelf ice hg.png|thumb|upright=1.6|Processes around an Antarctic ice shelf]]
[[File:Corp2400 - Flickr - NOAA Photo Library.jpg|thumb|The [[Ross Ice Shelf]] is Antarctica's largest. It is about the size of [[France]] and up to several hundred metres thick.]]
The large volume of ice on the Antarctic continent stores around 60% of the world's fresh water. Excluding [[groundwater]] this is 90%.<ref>{{cite web |title=Antarctic Factsheet |url=https://www.bas.ac.uk/science/science-and-society/education/antarctic-factsheet-geographical-statistics/ |publisher=British Antarctic Survey |access-date=15 January 2024}}</ref> Antarctica is experiencing ice loss from coastal glaciers in the [[West Antarctica]] and some glaciers of [[East Antarctica]]. However it is gaining mass from the increased snow build-up inland, particularly in the East. This leads to contradicting trends.<ref name="Zwally2021" /><ref name="NASA2023" /> There are different satellite methods for measuring ice mass and change. Combining them helps to reconcile the differences.<ref name="IMBIE2012">{{Cite journal|last1=Shepherd|first1=Andrew|last2=Ivins|first2=Erik|date=2012|title=A Reconciled Estimate of Ice-Sheet Mass Balance|url=http://www.escholarship.org/uc/item/0vq404h7|journal=[[Science (journal)|Science]]|volume=338|issue=6111|pages=1183–1189|bibcode=2012Sci...338.1183S|doi=10.1126/science.1228102|pmid=23197528|collaboration=[[Ice Sheet Mass Balance Inter-comparison Exercise|IMBIE]] team|hdl=2060/20140006608|s2cid=32653236}}</ref> However, there can still be variations between the studies. In 2018, a [[systematic review]] estimated average annual ice loss of 43 billion tons (Gt) across the entire continent between 1992 and 2002. This tripled to an annual average of 220 Gt from 2012 to 2017.<ref name="IMBIE2018">{{cite journal |title=Mass balance of the Antarctic Ice Sheet from 1992 to 2017 |journal=Nature |date=13 June 2018 |volume=558 |issue=7709 |pages=219–222 |doi=10.1038/s41586-018-0179-y |hdl=2268/225208 |pmid=29899482 |bibcode=2018Natur.558..219I |author1=IMBIE team |s2cid=49188002 |hdl-access=free}}</ref><ref>{{cite news |author=Scott K. Johnson |date=2018-06-13 |title=Latest estimate shows how much Antarctic ice has fallen into the sea |work=[[Ars Technica]] |url=https://arstechnica.com/science/2018/06/latest-estimate-shows-how-much-antarctic-ice-has-fallen-into-the-sea}}</ref> However, a 2021 analysis of data from four different research satellite systems ([[Envisat]], [[European Remote-Sensing Satellite]], [[GRACE and GRACE-FO]] and [[ICESat]]) indicated annual mass loss of only about 12 Gt from 2012 to 2016. This was due to greater ice gain in East Antarctica than estimated earlier.<ref name="Zwally2021" />

In the future, it is known that West Antarctica at least will continue to lose mass, and the likely future losses of sea ice and [[ice shelf|ice shelves]], which block warmer currents from direct contact with the ice sheet, can accelerate declines even in East Antarctica.<ref name="Greene2018" /><ref name="CNN_Jan2019">{{cite web|work=CNN|url=https://edition.cnn.com/2019/01/14/world/climate-change-antarctica-ice-melt-twin-studies/index.html|title=Antarctica ice melt has accelerated by 280% in the last 4 decades|date=14 January 2019 |access-date=January 14, 2019 |quote=Melting is taking place in the most vulnerable parts of Antarctica&nbsp;... parts that hold the potential for multiple metres of sea level rise in the coming century or two}}</ref> Altogether, Antarctica is the source of the largest uncertainty for future sea level projections.<ref name="Nature_20210505A">{{cite journal |last1=Edwards |first1=Tamsin L. |last2=Nowicki |first2=Sophie |last3=Marzeion |first3=Ben |last4=Hock |first4=Regine |last5=Goelzer |first5=Heiko |last6=Seroussi |first6=Hélène |display-authors=4 |date=5 May 2021 |title=Projected land ice contributions to twenty-first-century sea level rise |url=https://www.nature.com/articles/s41586-021-03302-y |journal=Nature |volume=593 |issue=7857 |pages=74–82 |bibcode=2021Natur.593...74E |doi=10.1038/s41586-021-03302-y |issn=0028-0836 |pmid=33953415 |hdl=1874/412157 |archive-url=https://web.archive.org/web/20210511000000/https://www.nature.com/articles/s41586-021-03302-y |archive-date=11 May 2021 |s2cid=233871029}} Alt URL https://eprints.whiterose.ac.uk/173870/</ref> In 2019, the [[Special Report on the Ocean and Cryosphere in a Changing Climate|SROCC]] assessed several studies attempting to estimate 2300 sea level rise caused by ice loss in Antarctica alone, arriving at projected estimates of {{Convert|0.07 - 0.37|m|ft}} for the low emission RCP2.6 scenario, and {{Convert|0.60 - 2.89|m|ft}} in the high emission RCP8.5 scenario.<ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1272}} This wide range of estimates is mainly due to the uncertainties regarding marine ice sheet and marine ice cliff instabilities.<ref name="Robel2019" /><ref name="Horton2020" /><ref name="Slangen2022" />

====East Antarctica====
{{Further|East Antarctic Ice Sheet}}
The world's largest potential source of sea level rise is the [[East Antarctic Ice Sheet]] (EAIS). It is 2.2&nbsp;km thick on average and holds enough ice to raise global sea levels by 53.3 m (174&nbsp;ft 10 in)<ref>{{cite journal |last1=Fretwell |first1=P. |last2=Pritchard |first2=H. D. |last3=Vaughan |first3=D. G. |last4=Bamber |first4=J. L. |last5=Barrand |first5=N. E. |last6=Bell |first6=R. |last7=Bianchi |first7=C. |last8=Bingham |first8=R. G. |last9=Blankenship |first9=D. D. |last10=Casassa |first10=G. |last11=Catania |first11=G. |last12=Callens |first12=D. |last13=Conway |first13=H. |last14=Cook |first14=A. J. |last15=Corr |first15=H. F. J. |last16=Damaske |first16=D. |last17=Damm |first17=V. |last18=Ferraccioli |first18=F. |last19=Forsberg |first19=R. |last20=Fujita |first20=S. |last21=Gim |first21=Y. |last22=Gogineni |first22=P. |last23=Griggs |first23=J. A. |last24=Hindmarsh |first24=R. C. A. |last25=Holmlund |first25=P. |last26=Holt |first26=J. W. |last27=Jacobel |first27=R. W. |last28=Jenkins |first28=A. |last29=Jokat |first29=W. |last30=Jordan |first30=T. |last31=King |first31=E. C. |last32=Kohler |first32=J. |last33=Krabill |first33=W. |last34=Riger-Kusk |first34=M. |last35=Langley |first35=K. A. |last36=Leitchenkov |first36=G. |last37=Leuschen |first37=C. |last38=Luyendyk |first38=B. P. |last39=Matsuoka |first39=K. |last40=Mouginot |first40=J. |last41=Nitsche |first41=F. O. |last42=Nogi |first42=Y. |last43=Nost |first43=O. A. |last44=Popov |first44=S. V. |last45=Rignot |first45=E. |last46=Rippin |first46=D. M. |last47=Rivera |first47=A. |last48=Roberts |first48=J. |last49=Ross |first49=N. |last50=Siegert |first50=M. J. |last51=Smith |first51=A. M. |last52=Steinhage |first52=D. |last53=Studinger |first53=M. |last54=Sun |first54=B. |last55=Tinto |first55=B. K. |last56=Welch |first56=B. C. |last57=Wilson |first57=D. |last58=Young |first58=D. A. |last59=Xiangbin |first59=C. |last60=Zirizzotti |first60=A. |title=Bedmap2: improved ice bed, surface and thickness datasets for Antarctica |journal=The Cryosphere |date=28 February 2013 |volume=7 |issue=1 |pages=375–393 |doi=10.5194/tc-7-375-2013 |bibcode=2013TCry....7..375F |doi-access=free}}</ref> Its great thickness and high elevation make it more stable than the other ice sheets.<ref name="Singh2020">{{Cite journal |last1=Singh |first1=Hansi A. |last2=Polvani |first2=Lorenzo M. |date=10 January 2020 |title=Low Antarctic continental climate sensitivity due to high ice sheet orography |journal=npj Climate and Atmospheric Science |language=en |volume=3 |issue=1 |page=39 |doi=10.1038/s41612-020-00143-w |s2cid=222179485 |doi-access=free |bibcode=2020npCAS...3...39S}}</ref> As of the early 2020s, most studies show that it is still gaining mass.<ref name="King2012">{{Cite journal | last1 = King | first1 = M. A. | last2 = Bingham | first2 = R. J. | last3 = Moore | first3 = P. | last4 = Whitehouse | first4 = P. L. | last5 = Bentley | first5 = M. J. | last6 = Milne | first6 = G. A. | doi = 10.1038/nature11621 | title = Lower satellite-gravimetry estimates of Antarctic sea-level contribution | journal = Nature | volume = 491 | issue = 7425 | pages = 586–589 | year = 2012 | pmid = 23086145|bibcode = 2012Natur.491..586K | s2cid = 4414976}}</ref><ref name="IMBIE2018"/><ref name="Zwally2021" /><ref name="NASA2023">{{cite web |title=Antarctic Ice Mass Loss 2002-2023 |url=https://svs.gsfc.nasa.gov/31158 |author=NASA |date=7 July 2023}}</ref> Some analyses have suggested it began to lose mass in the 2000s.<ref>{{cite journal |last1=Chen |first1=J. L. |last2=Wilson |first2=C. R. |last3=Blankenship |first3=D. |last4=Tapley |first4=B. D. |year=2009 |title=Accelerated Antarctic ice loss from satellite gravity measurements |journal=Nature Geoscience |volume=2 |issue=12 |pages=859 |doi=10.1038/ngeo694 |bibcode=2009NatGe...2..859C |s2cid=130927366}}</ref><ref name="Rignot2019">{{cite journal |last1=Rignot |first1=Eric |last2=Mouginot |first2=Jérémie |last3=Scheuchl |first3=Bernd |last4=van den Broeke |first4=Michiel |last5=van Wessem |first5=Melchior J. |last6=Morlighem |first6=Mathieu |title=Four decades of Antarctic Ice Sheet mass balance from 1979–2017 |journal=Proceedings of the National Academy of Sciences |date=22 January 2019 |volume=116 |issue=4 |pages=1095–1103 |doi=10.1073/pnas.1812883116 |pmid=30642972 |pmc=6347714 |bibcode=2019PNAS..116.1095R |doi-access=free}}</ref><ref name="CNN_Jan2019"/> However they over-extrapolated some observed losses on to the poorly observed areas. A more complete observational record shows continued mass gain.<ref name="Zwally2021">{{Cite journal |last1=Zwally |first1=H. Jay |last2=Robbins |first2=John W. |last3=Luthcke |first3=Scott B. |last4=Loomis |first4=Bryant D. |last5=Rémy |first5=Frédérique |date=29 March 2021 |title=Mass balance of the Antarctic ice sheet 1992–2016: reconciling results from GRACE gravimetry with ICESat, ERS1/2 and Envisat altimetry |journal=Journal of Glaciology |language=en |volume=67 |issue=263 |pages=533–559 |doi=10.1017/jog.2021.8 |bibcode=2021JGlac..67..533Z |quote=Although their methods of interpolation or extrapolation for areas with unobserved output velocities have an insufficient description for the evaluation of associated errors, such errors in previous results (Rignot and others, 2008) caused large overestimates of the mass losses as detailed in Zwally and Giovinetto (Zwally and Giovinetto, 2011).}}</ref>
[[File:Denman_oli_2020-057-059_lrg-labeled.svg|thumb|left|upright=1.4|Aerial view of ice flows at Denman Glacier, one of the less stable glaciers in the East Antarctica]]
In spite of the net mass gain, some East Antarctica glaciers have lost ice in recent decades due to [[ocean warming]] and declining structural support from the local [[sea ice]],<ref name="Greene2018">{{cite journal |last1=Greene |first1=Chad A. |last2=Young |first2=Duncan A. |last3=Gwyther |first3=David E. |last4=Galton-Fenzi |first4=Benjamin K. |last5=Blankenship |first5=Donald D. |title=Seasonal dynamics of Totten Ice Shelf controlled by sea ice buttressing |journal=The Cryosphere |date=6 September 2018 |volume=12 |issue=9 |pages=2869–2882 |doi=10.5194/tc-12-2869-2018 |bibcode=2018TCry...12.2869G |doi-access=free}}</ref> such as [[Denman Glacier]],<ref name="BrancatoRignot2020">{{cite journal|last1=Brancato |first1=V. |last2=Rignot |first2=E. |last3=Milillo |first3=P. |last4=Morlighem |first4=M. |last5=Mouginot |first5=J. |last6=An |first6=L. |last7=Scheuchl |first7=B. |last8=Jeong |first8=S. |last9=Rizzoli |first9=P. |last10=Bueso Bello |first10=J.L. |last11=Prats-Iraola |first11=P. |title=Grounding line retreat of Denman Glacier, East Antarctica, measured with COSMO-SkyMed radar interferometry data |journal=Geophysical Research Letters |year=2020 |volume=47 |issue=7 |pages=e2019GL086291|issn=0094-8276 |doi=10.1029/2019GL086291 |bibcode=2020GeoRL..4786291B |doi-access=free}}</ref><ref>{{cite news|newspaper=[[BBC]]|url=https://www.bbc.com/news/science-environment-52007637|title=Climate change: Earth's deepest ice canyon vulnerable to melting |last=Amos|first=Jonathan|date=2020-03-23}}</ref> and [[Totten Glacier]].<ref>{{cite journal |last1=Greene |first1=Chad A. |last2=Blankenship |first2=Donald D. |last3=Gwyther |first3=David E. |last4=Silvano |first4=Alessandro |last5=van Wijk |first5=Esmee |title=Wind causes Totten Ice Shelf melt and acceleration |journal=Science Advances |date=1 November 2017 |volume=3 |issue=11 |pages=e1701681 |doi=10.1126/sciadv.1701681 |pmid=29109976 |pmc=5665591 |bibcode=2017SciA....3E1681G}}</ref><ref>{{cite journal |last1=Roberts |first1=Jason |last2=Galton-Fenzi |first2=Benjamin K. |last3=Paolo |first3=Fernando S. |last4=Donnelly |first4=Claire |last5=Gwyther |first5=David E. |last6=Padman |first6=Laurie |last7=Young |first7=Duncan |last8=Warner |first8=Roland |last9=Greenbaum |first9=Jamin |last10=Fricker |first10=Helen A. |last11=Payne |first11=Antony J. |last12=Cornford |first12=Stephen |last13=Le Brocq |first13=Anne |last14=van Ommen |first14=Tas |last15=Blankenship |first15=Don |last16=Siegert |first16=Martin J. |title=Ocean forced variability of Totten Glacier mass loss |journal=Geological Society, London, Special Publications |date=2018 |volume=461 |issue=1 |pages=175–186 |doi=10.1144/sp461.6 |bibcode=2018GSLSP.461..175R |s2cid=55567382 |url=https://research-information.bristol.ac.uk/en/publications/ocean-forced-variability-of-totten-glacier-mass-loss(27694a07-b3c7-45fd-bdfb-74eb6b09c3e0).html |doi-access=free}}</ref> Totten Glacier is particularly important because it stabilizes the [[Aurora Subglacial Basin]]. Subglacial basins like Aurora and [[Wilkes Basin]] are major ice reservoirs together holding as much ice as all of West Antarctica.<ref>{{cite journal |last1=Greenbaum |first1=J. S. |last2=Blankenship |first2=D. D. |last3=Young |first3=D. A. |last4=Richter |first4=T. G. |last5=Roberts |first5=J. L. |last6=Aitken |first6=A. R. A. |last7=Legresy |first7=B. |last8=Schroeder |first8=D. M. |last9=Warner |first9=R. C. |last10=van Ommen |first10=T. D. |last11=Siegert |first11=M. J. |title=Ocean access to a cavity beneath Totten Glacier in East Antarctica |journal=Nature Geoscience |date=16 March 2015 |volume=8 |issue=4 |pages=294–298 |doi=10.1038/ngeo2388 |bibcode=2015NatGe...8..294G}}</ref> They are more vulnerable than the rest of East Antarctica.<ref name="Pollard2015">{{cite journal |last1=Pollard |first1=David |last2=DeConto |first2=Robert M. |last3=Alley |first3=Richard B. |title=Potential Antarctic Ice Sheet retreat driven by hydrofracturing and ice cliff failure |journal=Earth and Planetary Science Letters |date=February 2015 |volume=412 |pages=112–121 |doi=10.1016/j.epsl.2014.12.035 |bibcode=2015E&PSL.412..112P |doi-access=free}}</ref> Their collective [[tipping points in the climate system|tipping point]] probably lies at around {{convert|3|C-change|F-change}} of global warming. It may be as high as {{convert|6|C-change|F-change}} or as low as {{convert|2|C-change|F-change}}. Once this tipping point is crossed, the collapse of these subglacial basins could take place over as little as 500 or as much as 10,000 years. The median timeline is 2000 years.<ref name="ArmstrongMcKay2022" /><ref name="ArmstrongMcKayExplainer" /> Depending on how many subglacial basins are vulnerable, this causes sea level rise of between {{convert|1.4|m|ftin|abbr=on}} and {{convert|6.4|m|ftin|abbr=on}}.<ref name="Pan2021">{{Cite journal|last1=Pan |first1=Linda |last2=Powell |first2=Evelyn M. |last3=Latychev |first3=Konstantin |last4=Mitrovica |first4=Jerry X. |last5=Creveling |first5=Jessica R. |last6=Gomez |first6=Natalya |last7=Hoggard |first7=Mark J. |last8=Clark |first8=Peter U. |date=30 April 2021 |title=Rapid postglacial rebound amplifies global sea level rise following West Antarctic Ice Sheet collapse |journal=Science Advances |volume=7 |issue=18 |doi=10.1126/sciadv.abf7787 |pmid=33931453 |pmc=8087405 |bibcode=2021SciA....7.7787P}}</ref>

On the other hand, the whole EAIS would not definitely collapse until global warming reaches {{convert|7.5|C-change|F-change}}, with a range between {{convert|5|C-change|F-change}} and {{convert|10|C-change|F-change}}. It would take at least 10,000 years to disappear.<ref name="ArmstrongMcKay2022" /><ref name="ArmstrongMcKayExplainer" /> Some scientists have estimated that warming would have to reach at least {{convert|6|C-change|F-change}} to melt two thirds of its volume.<ref name="Garbe2020">{{Cite journal |last1=Garbe |first1=Julius |last2=Albrecht |first2=Torsten |last3=Levermann |first3=Anders |last4=Donges |first4=Jonathan F. |last5=Winkelmann |first5=Ricarda |date=2020 |title=The hysteresis of the Antarctic Ice Sheet |url=https://www.nature.com/articles/s41586-020-2727-5 |journal=Nature |volume=585 |issue=7826 |pages=538–544 |doi=10.1038/s41586-020-2727-5|pmid=32968257 |bibcode=2020Natur.585..538G |s2cid=221885420}}</ref>

====West Antarctica====
{{Further|West Antarctic Ice Sheet}}
[[File:Thwaites Glacier.jpg|thumb|upright=1.35|Thwaites Glacier, with its vulnerable bedrock topography visible.]]
East Antarctica contains the largest potential source of sea level rise. However the [[West Antarctic Ice Sheet|West Antarctic ice sheet]] (WAIS) is substantially more vulnerable. Temperatures on West Antarctica have increased significantly, unlike East Antarctica and the [[Antarctic Peninsula]]. The trend is between {{convert|0.08|C-change|F-change}} and {{convert|0.96|C-change|F-change}} per decade between 1976 and 2012.<ref>{{cite journal |last1=Ludescher |first1=Josef |last2=Bunde |first2=Armin |last3=Franzke |first3=Christian L. E. |last4=Schellnhuber |first4=Hans Joachim |title=Long-term persistence enhances uncertainty about anthropogenic warming of Antarctica |journal=Climate Dynamics |date=16 April 2015 |volume=46 |issue=1–2 |pages=263–271 |doi=10.1007/s00382-015-2582-5 |bibcode=2016ClDy...46..263L |s2cid=131723421}}</ref> Satellite observations recorded a substantial increase in WAIS melting from 1992 to 2017. This resulted in {{Convert|7.6 ± 3.9|mm|in|frac=64|abbr=on}} of Antarctica sea level rise. Outflow glaciers in the [[Amundsen Sea Embayment]] played a disproportionate role.<ref name="RignotBamber2008">{{cite journal |last1=Rignot |first1=Eric |last2=Bamber |first2=Jonathan L. |last3=van den Broeke |first3=Michiel R. |last4=Davis |first4=Curt |last5=Li |first5=Yonghong |last6=van de Berg |first6=Willem Jan |last7=van Meijgaard |first7=Erik |title=Recent Antarctic ice mass loss from radar interferometry and regional climate modelling |journal=Nature Geoscience |date=13 January 2008 |volume=1 |issue=2 |pages=106–110 |doi=10.1038/ngeo102 |bibcode=2008NatGe...1..106R |s2cid=784105 |url=http://www.escholarship.org/uc/item/26f4j9vv}}</ref>

[[File:West Antarctic Collapse.ogv|thumb|upright=1.35|left|A graphical representation of how warm waters, and the Marine Ice Sheet Instability and Marine Ice Cliff Instability processes are affecting the West Antarctic Ice Sheet]]

The ''median'' estimated increase in sea level rise from Antarctica by 2100 is ~{{convert|11|cm|in|round=5|abbr=on}}. There is no difference between scenarios, because the increased warming would [[effects of climate change on the water cycle|intensify the water cycle]] and increase [[snowfall]] accumulation over the EAIS at about the same rate as it would increase ice loss from WAIS.<ref name="IPCC AR6 WG1 Ch.9" /> However, most of the [[bedrock]] underlying the WAIS lies well below sea level, and it has to be buttressed by the [[Thwaites glacier|Thwaites]] and [[Pine Island glacier|Pine Island]] glaciers. If these glaciers were to collapse, the entire ice sheet would as well.<ref name="Pollard2015"/> Their disappearance would take at least several centuries, but is considered almost inevitable, as their bedrock [[topography]] deepens inland and becomes more vulnerable to meltwater, in what is known as marine ice sheet instability.<ref name="Robel2019">{{cite journal |last1=Robel |first1=Alexander A. |last2=Seroussi |first2=Hélène |last3=Roe |first3=Gerard H. |title=Marine ice sheet instability amplifies and skews uncertainty in projections of future sea-level rise |journal=Proceedings of the National Academy of Sciences |date=23 July 2019 |volume=116 |issue=30 |pages=14887–14892 |doi=10.1073/pnas.1904822116 |pmid=31285345 |pmc=6660720 |bibcode=2019PNAS..11614887R |doi-access=free}}</ref> <ref name="Pettit2021">{{Cite web |last1=Voosen |first1=Paul |date=13 December 2021 |title=Ice shelf holding back keystone Antarctic glacier within years of failure|url=https://www.science.org/content/article/ice-shelf-holding-back-keystone-antarctic-glacier-within-years-failure|access-date=2022-10-22|website=[[Science Magazine]]|language=en|quote=Because Thwaites sits below sea level on ground that dips away from the coast, the warm water is likely to melt its way inland, beneath the glacier itself, freeing its underbelly from bedrock. A collapse of the entire glacier, which some researchers think is only centuries away, would raise global sea level by 65 centimeters.}}</ref><ref name=BBC1 >{{cite news |last=Amos |first=Jonathan |date=13 December 2021 |title=Thwaites: Antarctic glacier heading for dramatic change |url=https://www.bbc.com/news/science-environment-59644494 |work=[[BBC News]] |location=London |access-date=December 14, 2021}}</ref>

The contribution of these glaciers to global sea levels has already accelerated since the year 2000. The Thwaites Glacier now accounts for 4% of global sea level rise.<ref name="Pettit2021" /><ref>{{cite web|url=https://www.theatlantic.com/science/archive/2018/06/after-decades-of-ice-loss-antarctica-is-now-hemorrhaging-mass/562748/|work=The Atlantic|year=2018|title=After Decades of Losing Ice, Antarctica Is Now Hemorrhaging It}}</ref><ref>{{cite web|url=http://www.antarcticglaciers.org/glaciers-and-climate/ice-ocean-interactions/marine-ice-sheets/|work=AntarcticGlaciers.org|year=2014|title=Marine ice sheet instability}}</ref> It could start to lose even more ice if the [[Thwaites Ice Shelf]] fails and would no longer stabilize it, which could potentially occur in mid-2020s.<ref name=Kaplan1>{{cite news |last=Kaplan |first=Sarah |date=December 13, 2021 |title=Crucial Antarctic ice shelf could fail within five years, scientists say |url=https://www.washingtonpost.com/climate-environment/2021/12/13/thwaites-glacier-melt-antarctica/ |newspaper=[[The Washington Post]] |location=Washington DC |access-date=December 14, 2021}}</ref> A combination of ice sheet instability with other important but hard-to-model processes like hydrofracturing (meltwater collects atop the ice sheet, pools into fractures and forces them open)<ref name="pmid30013142">{{cite journal |last1=Pattyn |first1=Frank |author-link=Frank Pattyn |date=16 July 2018 |title=The paradigm shift in Antarctic ice sheet modelling |journal=Nature Communications |volume=9 |issue=1 |page=2728 |bibcode=2018NatCo...9.2728P |doi=10.1038/s41467-018-05003-z |pmc=6048022 |pmid=30013142}}</ref> or smaller-scale changes in ocean circulation<ref>{{Cite journal |last1=Golledge |first1=Nicholas R. |last2=Keller |first2=Elizabeth D. |last3=Gomez |first3=Natalya |last4=Naughten |first4=Kaitlin A. |last5=Bernales |first5=Jorge |last6=Trusel |first6=Luke D. |last7=Edwards |first7=Tamsin L. |date=2019 |title=Global environmental consequences of twenty-first-century ice-sheet melt |journal=Nature |language=en |volume=566 |issue=7742 |pages=65–72 |doi=10.1038/s41586-019-0889-9 |pmid=30728520 |bibcode=2019Natur.566...65G |s2cid=59606358 |issn=1476-4687}}</ref><ref>{{Cite journal |last1=Moorman |first1=Ruth |last2=Morrison |first2=Adele K. |last3=Hogg |first3=Andrew McC |date=2020-08-01 |title=Thermal Responses to Antarctic Ice Shelf Melt in an Eddy-Rich Global Ocean–Sea Ice Model |journal=Journal of Climate |language=EN |volume=33 |issue=15 |pages=6599–6620 |doi=10.1175/JCLI-D-19-0846.1 |bibcode=2020JCli...33.6599M |s2cid=219487981 |issn=0894-8755}}</ref><ref name="Naughten2023" /> could cause the WAIS to contribute up to {{convert|41|cm|in|0|abbr=on}} by 2100 under the low-emission scenario and up to {{convert|57|cm|in|0|abbr=on}} under the highest-emission one.<ref name="IPCC AR6 WG1 Ch.9" /> Ice cliff instability would cause a contribution of {{cvt|1|m|ft|frac=2}} or more if it were applicable.<ref name="DeConto2016" /><ref name="Kopp2023" />

The melting of all the [[ice]] in West Antarctica would increase the total sea level rise to {{convert|4.3|m|ftin|abbr=on}}.<ref name="BEDMAP2-2013">{{cite journal |last1=Fretwell |first1=P. |display-authors=et al |title=Bedmap2: improved ice bed, surface and thickness datasets for Antarctica |journal=The Cryosphere |volume=7 |issue=1 |page=390 |date=28 February 2013 |url=http://www.the-cryosphere.net/7/375/2013/tc-7-375-2013.pdf |access-date=6 January 2014 |doi=10.5194/tc-7-375-2013 |bibcode=2013TCry....7..375F |s2cid=13129041 |doi-access=free |archive-date=16 February 2020 |archive-url=https://web.archive.org/web/20200216072841/https://www.the-cryosphere.net/7/375/2013/tc-7-375-2013.pdf |url-status=live}}</ref> However, mountain [[ice cap]]s not in contact with water are less vulnerable than the majority of the ice sheet, which is located below the sea level.<ref name="Hein2016">{{Cite journal |last1=Hein |first1=Andrew S. |last2=Woodward |first2=John |last3=Marrero |first3=Shasta M. |last4=Dunning |first4=Stuart A. |last5=Steig |first5=Eric J. |last6=Freeman |first6=Stewart P. H. T. |last7=Stuart |first7=Finlay M. |last8=Winter |first8=Kate |last9=Westoby |first9=Matthew J. |last10=Sugden |first10=David E. |date=3 February 2016 |title=Evidence for the stability of the West Antarctic Ice Sheet divide for 1.4 million years |journal=Nature Communications |volume=7 |page=10325 |doi=10.1038/ncomms10325 |pmid=26838462 |pmc=4742792 |bibcode=2016NatCo...710325H}}</ref> Its collapse would cause ~{{convert|3.3|m|ftin|abbr=on}} of sea level rise.<ref name="Bamber2009">{{cite journal |last1=Bamber |first1=J.L. |last2=Riva |first2=R.E.M. |last3=Vermeersen |first3=B.L.A. |last4=LeBrocq |first4=A.M. |title=Reassessment of the Potential Sea-Level Rise from a Collapse of the West Antarctic Ice Sheet |journal=Science |date=14 May 2009 |volume=324 |issue=5929 |pages=901–903 |doi=10.1126/science.1169335 |pmid=19443778 |bibcode=2009Sci...324..901B |s2cid=11083712}}</ref> This collapse appears to have already occurred during the [[Eemian]] period 125,000 years ago, when temperatures were similar to the early 21st century, so it is likely to be inevitable at this stage.<ref>{{Cite web|url=https://www.science.org/content/article/discovery-recent-antarctic-ice-sheet-collapse-raises-fears-new-global-flood|title=Discovery of recent Antarctic ice sheet collapse raises fears of a new global flood|last=Voosen|first=Paul|date=2018-12-18|website=Science|language=en|access-date=2018-12-28}}</ref><ref>{{Cite journal|last1=Turney|first1=Chris S. M.|last2=Fogwill|first2=Christopher J.|last3=Golledge|first3=Nicholas R.|last4=McKay |first4=Nicholas P. |last5=Sebille |first5=Erik van |last6=Jones |first6=Richard T. |last7=Etheridge |first7=David|last8=Rubino |first8=Mauro|last9=Thornton|first9=David P. |last10=Davies|first10=Siwan M.|last11=Ramsey|first11=Christopher Bronk|date=2020-02-11|title=Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica|journal=Proceedings of the National Academy of Sciences |volume=117 |issue=8 |pages=3996–4006 |language=en |doi=10.1073/pnas.1902469117|issn=0027-8424 |pmid=32047039 |pmc=7049167 |bibcode=2020PNAS..117.3996T|doi-access=free}}</ref><ref name="Carlson2018">{{Cite conference |last1=Carlson |first1=Anders E |last2=Walczak |first2=Maureen H |last3=Beard |first3=Brian L |last4=Laffin |first4=Matthew K |last5=Stoner |first5=Joseph S |last6=Hatfield |first6=Robert G |date=10 December 2018 |title=Absence of the West Antarctic ice sheet during the last interglaciation |url=https://agu.confex.com/agu/fm18/meetingapp.cgi/Paper/421418 |conference=American Geophysical Union Fall Meeting}}</ref><ref name="Lau2023">{{Cite journal |last1=Lau |first1=Sally C. Y. |last2=Wilson |first2=Nerida G. |last3=Golledge |first3=Nicholas R. |last4=Naish |first4=Tim R. |last5=Watts |first5=Phillip C. |last6=Silva |first6=Catarina N. S. |last7=Cooke |first7=Ira R. |last8=Allcock |first8=A. Louise |last9=Mark |first9=Felix C. |last10=Linse |first10=Katrin |date=21 December 2023 |title=Genomic evidence for West Antarctic Ice Sheet collapse during the Last Interglacial |journal=Science |language=en |volume=382 |issue=6677 |pages=1384–1389 |doi=10.1126/science.ade0664 |pmid=38127761 |bibcode=2023Sci...382.1384L |s2cid=266436146 |url=https://epic.awi.de/id/eprint/58369/1/science.ade0664%281%29.pdf}}</ref><ref>{{Cite web |last=AHMED |first=Issam |title=Antarctic octopus DNA reveals ice sheet collapse closer than thought |url=https://phys.org/news/2023-12-antarctic-octopus-dna-reveals-ice.html |access-date=2023-12-23 |website=phys.org |language=en}}</ref><ref name="Naughten2023">{{cite journal |last1=A. Naughten |first1=Kaitlin |last2=R. Holland |first2=Paul |last3=De Rydt |first3=Jan|title=Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century |journal=Nature Climate Change |date=23 October 2023 |volume=13 |issue=11 |pages=1222–1228 |doi=10.1038/s41558-023-01818-x |s2cid=264476246 |doi-access=free |bibcode=2023NatCC..13.1222N}}</ref><ref>{{cite news |last1=Poynting |first1=Mark |title=Sea-level rise: West Antarctic ice shelf melt 'unavoidable' |url=https://www.bbc.com/news/science-environment-67171231 |access-date=26 October 2023 |agency=BBC |date=24 October 2023}}</ref> This disappearance would take an estimated 2000 years. The absolute minimum for the loss of West Antarctica ice is 500 years, and the potential maximum is 13,000 years.<ref name="ArmstrongMcKay2022">{{Cite journal |last1=Armstrong McKay |first1=David|last2=Abrams |first2=Jesse |last3=Winkelmann |first3=Ricarda |last4=Sakschewski |first4=Boris |last5=Loriani |first5=Sina |last6=Fetzer |first6=Ingo|last7=Cornell|first7=Sarah |last8=Rockström |first8=Johan |last9=Staal |first9=Arie |last10=Lenton |first10=Timothy |date=9 September 2022 |title=Exceeding 1.5°C global warming could trigger multiple climate tipping points |url=https://www.science.org/doi/10.1126/science.abn7950 |journal=Science |language=en |volume=377 |issue=6611 |pages=eabn7950 |doi=10.1126/science.abn7950 |pmid=36074831 |hdl=10871/131584 |s2cid=252161375 |issn=0036-8075}}</ref><ref name="ArmstrongMcKayExplainer">{{Cite web |last=Armstrong McKay |first=David |date=9 September 2022 |title=Exceeding 1.5°C global warming could trigger multiple climate tipping points – paper explainer |url=https://climatetippingpoints.info/2022/09/09/climate-tipping-points-reassessment-explainer/ |access-date=2 October 2022 |website=climatetippingpoints.info |language=en}}</ref>

Once ice loss from the West Antarctica is triggered, the only way to restore it to near-present values is by lowering the global temperature to {{convert|1|C-change|F-change}} ''below'' the preindustrial level. This would be {{convert|2|C-change|F-change}} below the temperature of 2020.<ref name="Garbe2020" /> Other researchers suggested that a [[climate engineering]] intervention to stabilize the ice sheet's glaciers may delay its loss by centuries and give more time to adapt. However this is an uncertain proposal, and would end up as one of the most expensive projects ever attempted.<ref name="Wolovick2023a">{{Cite journal |last1=Wolovick |first1=Michael |last2=Moore |first2=John |last3=Keefer |first3=Bowie |date=27 March 2023 |title=Feasibility of ice sheet conservation using seabed anchored curtains |url=https://academic.oup.com/pnasnexus/article/2/4/pgad103/7087219 |journal=PNAS Nexus |volume=2 |issue=3 |pages=pgad053 |language=en |doi=10.1093/pnasnexus/pgad053 |pmid=37007716 |pmc=10062297}}</ref><ref name="Wolovick2023b">{{Cite journal |last1=Wolovick |first1=Michael |last2=Moore |first2=John |last3=Keefer |first3=Bowie |date=27 March 2023 |title=The potential for stabilizing Amundsen Sea glaciers via underwater curtains |url=https://academic.oup.com/pnasnexus/article/2/4/pgad103/7087219 |journal=PNAS Nexus |volume=2 |issue=4 |pages=pgad103 |language=en |doi=10.1093/pnasnexus/pgad103 |pmid=37091546 |pmc=10118300}}</ref>

====Isostatic rebound====
2021 research indicates that [[isostatic rebound]] after the loss of the main portion of the West Antarctic ice sheet would ultimately add another {{convert|1.02|m|ftin|abbr=on}} to global sea levels. This effect would start to increase sea levels before 2100. However it would take 1000 years for it to cause {{convert|83|cm|ftin|abbr=on}} of sea level rise. At this point, West Antarctica itself would be {{convert|610|m|ftin|abbr=on}} higher than now. Estimates of isostatic rebound after the loss of East Antarctica's subglacial basins suggest SLR contributions of between {{convert|8|cm|ftin|abbr=on}} and {{convert|57|cm|ftin|abbr=on}}<ref name="Pan2021" />

[[File:Mass changes of the Greenland Ice Sheet between 2002 and 2019.webp|thumb|Trends of Greenland ice loss between 2002 and 2019<ref>{{cite journal |last1=Sasgen |first1=Ingo |last2=Wouters |first2=Bert |last3=Gardner |first3=Alex S. |last4=King |first4=Michalea D. |last5=Tedesco |first5=Marco |last6=Landerer |first6=Felix W. |last7=Dahle |first7=Christoph |last8=Save |first8=Himanshu |last9=Fettweis |first9=Xavier |date=20 August 2020 |title=Return to rapid ice loss in Greenland and record loss in 2019 detected by the GRACE-FO satellites |journal=Communications Earth & Environment |volume=1 |issue=1 |page=8 |doi=10.1038/s43247-020-0010-1 |bibcode=2020ComEE...1....8S |s2cid=221200001 |language=en |issn=2662-4435|doi-access=free}} [[File:CC-BY icon.svg|50px]] Text and images are available under a [https://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International License].</ref>]]

=== Greenland ice sheet loss ===
Most ice on Greenland is in the [[Greenland ice sheet]] which is {{Convert|3|km|ft|abbr=on|sigfig=1}} at its thickest. The rest of Greenland ice forms isolated glaciers and ice caps. The average annual ice loss in Greenland more than doubled in the early 21st century compared to the 20th century.<ref>{{cite journal |last1=Kjeldsen |first1=Kristian K. |last2=Korsgaard |first2=Niels J. |last3=Bjørk |first3=Anders A. |last4=Khan |first4=Shfaqat A. |last5=Box |first5=Jason E. |last6=Funder |first6=Svend |last7=Larsen |first7=Nicolaj K. |last8=Bamber |first8=Jonathan L. |last9=Colgan |first9=William |last10=van den Broeke |first10=Michiel |last11=Siggaard-Andersen |first11=Marie-Louise |last12=Nuth |first12=Christopher |last13=Schomacker |first13=Anders |last14=Andresen |first14=Camilla S. |last15=Willerslev |first15=Eske |last16=Kjær |first16=Kurt H. |title=Spatial and temporal distribution of mass loss from the Greenland Ice Sheet since AD 1900 |journal=Nature |date=16 December 2015 |volume=528 |issue=7582 |pages=396–400 |doi=10.1038/nature16183 |pmid=26672555 |bibcode=2015Natur.528..396K |hdl=10852/50174 |s2cid=4468824 |url=https://research-information.bris.ac.uk/en/publications/spatial-and-temporal-distribution-of-mass-loss-from-the-greenland-ice-sheet-since-ad-1900(29ed76ed-b8f7-4b99-bf59-a275b0a22ce7).html}}</ref> Its contribution to sea level rise correspondingly increased from 0.07&nbsp;mm per year between 1992 and 1997 to 0.68&nbsp;mm per year between 2012 and 2017. Total ice loss from the Greenland ice sheet between 1992 and 2018 amounted to 3,902 gigatons (Gt) of ice. This is equivalent to a SLR contribution of 10.8&nbsp;mm.<ref>{{Cite journal|last1=Shepherd|first1=Andrew|last2=Ivins|first2=Erik|last3=Rignot|first3=Eric|last4=Smith|first4=Ben|last5=van den Broeke|first5=Michiel|last6=Velicogna|first6=Isabella|author-link6=Isabella Velicogna|last7=Whitehouse|first7=Pippa|last8=Briggs|first8=Kate|last9=Joughin|first9=Ian|last10=Krinner|first10=Gerhard|last11=Nowicki|first11=Sophie|date=2020-03-12|title=Mass balance of the Greenland Ice Sheet from 1992 to 2018|journal=Nature|language=en|volume=579|issue=7798|pages=233–239|doi=10.1038/s41586-019-1855-2|pmid=31822019|hdl=2268/242139|s2cid=219146922|issn=1476-4687|url=https://orbi.uliege.be/handle/2268/242139}}</ref> The contribution for the 2012–2016 period was equivalent to 37% of sea level rise from ''land ice'' sources (excluding thermal expansion).<ref name="Bamber2018">{{cite journal |last1=Bamber |first1=Jonathan L |last2=Westaway |first2=Richard M |last3=Marzeion |first3=Ben |last4=Wouters |first4=Bert |title=The land ice contribution to sea level during the satellite era |journal=Environmental Research Letters |date=1 June 2018 |volume=13 |issue=6 |page=063008 |doi=10.1088/1748-9326/aac2f0 |bibcode=2018ERL....13f3008B |doi-access=free}}</ref> This observed rate of ice sheet melting is at the higher end of predictions from past [[IPCC]] assessment reports.<ref>{{Cite web|url=https://news.uci.edu/2019/12/19/greenland-ice-loss-is-at-worse-case-scenario-levels-study-finds/|title=Greenland ice loss is at 'worse-case scenario' levels, study finds|date=2019-12-19|website=UCI News|language=en-US|access-date=2019-12-28}}</ref><ref name="Slater-2020"/> 
[[File:Beckmann 2023 Greenland 2300 RCP85 extent.png|thumb|left|2023 projections of how much the Greenland ice sheet may shrink from its present extent by the year 2300 under the worst possible climate change scenario (upper half) and of how much faster its remaining ice will be flowing in that case (lower half)<ref name="Beckmann2023">{{Cite journal |last1=Beckmann |first1=Johanna |last2=Winkelmann |first2=Ricarda |date=27 July 2023 |title=Effects of extreme melt events on ice flow and sea level rise of the Greenland Ice Sheet |journal=The Cryosphere |language=en |volume=17 |issue=7 |pages=3083–3099 |doi=10.5194/tc-17-3083-2023 |bibcode=2023TCry...17.3083B |doi-access=free}}</ref>]]
In 2021, [[AR6]] estimated that by 2100, the melting of Greenland ice sheet would most likely add around {{cvt|6|cm|in|frac=2}} to sea levels under the low-emission scenario, and {{cvt|13|cm|in|frac=2}} under the high-emission scenario. The first scenario, [[Shared Socioeconomic Pathways|SSP1-2.6]], largely fulfils the [[Paris Agreement]] goals, while the other, SSP5-8.5, has the emissions accelerate throughout the century. The uncertainty about [[ice sheet dynamics]] can affect both pathways. In the best-case scenario, ice sheet under SSP1-2.6 gains enough mass by 2100 through [[surface mass balance]] feedbacks to reduce the sea levels by {{cvt|2|cm|in|frac=2}}. In the worst case, it adds {{cvt|15|cm|in|frac=2}}. For SSP5-8.5, the best-case scenario is adding {{cvt|5|cm|in|frac=2}} to sea levels, and the worst-case is adding {{cvt|23|cm|in|frac=2}}.<ref name="IPCC AR6 WG1 Ch.9" />{{Rp|page=1260}}

Greenland's peripheral glaciers and ice caps crossed an irreversible tipping point around 1997. Sea level rise from their loss is now unstoppable.<ref>{{cite journal |last1=Noël |first1=B. |last2=van de Berg |first2=W. J |last3=Lhermitte |first3=S. |last4=Wouters |first4=B. |last5=Machguth |first5=H. |last6=Howat |first6=I. |last7=Citterio |first7=M. |last8=Moholdt |first8=G. |last9=Lenaerts |first9=J. T. M. |last10=van den Broeke |first10=M. R. |title=A tipping point in refreezing accelerates mass loss of Greenland's glaciers and ice caps |journal=Nature Communications |date=31 March 2017 |volume=8 |issue=1 |page=14730 |doi=10.1038/ncomms14730 |pmid=28361871 |pmc=5380968 |bibcode=2017NatCo...814730N}}</ref><ref>{{cite news |title=Warming Greenland ice sheet passes point of no return|url=https://news.osu.edu/warming-greenland-ice-sheet-passes-point-of-no-return/|date=13 August 2020|access-date=15 August 2020 |work=Ohio State University}}</ref><ref>{{cite journal|last1=King|first1=Michalea D.|last2=Howat|first2=Ian M.|last3=Candela|first3=Salvatore G.|last4=Noh|first4=Myoung J.|last5=Jeong|first5=Seongsu|last6=Noël|first6=Brice P. Y.|last7=van den Broeke|first7=Michiel R.|last8=Wouters|first8=Bert|last9=Negrete|first9=Adelaide|date=13 August 2020|title=Dynamic ice loss from the Greenland Ice Sheet driven by sustained glacier retreat|journal=Communications Earth & Environment|language=en|volume=1|issue=1|pages=1–7|doi=10.1038/s43247-020-0001-2|bibcode=2020ComEE...1....1K |issn=2662-4435|doi-access=free}} [[File:CC-BY icon.svg|50x50px]] Text and images are available under a [[creativecommons:by/4.0/|Creative Commons Attribution 4.0 International License]].</ref> However the temperature changes in future, the warming of 2000–2019 had already damaged the ice sheet enough for it to eventually lose ~3.3% of its volume. This is leading to {{cvt|27|cm|in|frac=2}} of future sea level rise.<ref>{{cite journal |last1=Box |first1=Jason E. |last2=Hubbard |first2=Alun |last3=Bahr |first3=David B. |last4=Colgan |first4=William T. |last5=Fettweis |first5=Xavier |last6=Mankoff |first6=Kenneth D. |last7=Wehrlé |first7=Adrien |last8=Noël |first8=Brice |last9=van den Broeke |first9=Michiel R. |last10=Wouters |first10=Bert |last11=Bjørk |first11=Anders A. |last12=Fausto |first12=Robert S. |title=Greenland ice sheet climate disequilibrium and committed sea-level rise |url=https://www.nature.com/articles/s41558-022-01441-2 |journal=Nature Climate Change |date=29 August 2022 |volume=12 |issue=9 |pages=808–813 |doi=10.1038/s41558-022-01441-2 |bibcode=2022NatCC..12..808B |s2cid=251912711}}</ref> At a certain level of global warming, the Greenland ice sheet will almost completely melt. Ice cores show this happened at least once during the last million years, when the temperatures have at most been {{convert|2.5|C-change|F-change}} warmer than the preindustrial.<ref>{{Cite journal|last1=Irvalı|first1=Nil|last2=Galaasen|first2=Eirik V.|last3=Ninnemann|first3=Ulysses S.|last4=Rosenthal|first4=Yair|last5=Born|first5=Andreas|last6=Kleiven|first6=Helga (Kikki) F.|date=18 December 2019 |title=A low climate threshold for south Greenland Ice Sheet demise during the Late Pleistocene|journal=Proceedings of the National Academy of Sciences|volume=117|issue=1|pages=190–195|language=en|doi=10.1073/pnas.1911902116|issn=0027-8424|pmid=31871153|pmc=6955352|doi-access=free}}</ref><ref name="Christ2021">{{cite journal |last1=Christ |first1=Andrew J. |last2=Bierman |first2=Paul R. |last3=Schaefer |first3=Joerg M.|last4=Dahl-Jensen |first4=Dorthe |last5=Steffensen |first5=Jørgen P. |last6=Corbett |first6=Lee B. |last7=Peteet |first7=Dorothy M. |last8=Thomas |first8=Elizabeth K. |last9=Steig |first9=Eric J. |last10=Rittenour |first10=Tammy M. |last11=Tison |first11=Jean-Louis |last12=Blard |first12=Pierre-Henri |last13=Perdrial |first13=Nicolas |last14=Dethier |first14=David P. |last15=Lini |first15=Andrea |last16=Hidy |first16=Alan J. |last17=Caffee |first17=Marc W. |last18=Southon |first18=John |title=A multimillion-year-old record of Greenland vegetation and glacial history preserved in sediment beneath 1.4 km of ice at Camp Century |journal=Proceedings of the National Academy of Sciences of the United States|date=30 March 2021 |volume=118 |issue=13 |pages=e2021442118 |doi=10.1073/pnas.2021442118 |pmid=33723012 |pmc=8020747 |bibcode=2021PNAS..11821442C |doi-access=free}}</ref>

2012 research suggested that the tipping point of the ice sheet was between {{convert|0.8|C-change|F-change}} and {{convert|3.2|C-change|F-change}}.<ref>{{cite journal |last1=Robinson |first1=Alexander |last2=Calov |first2=Reinhard |last3=Ganopolski |first3=Andrey |title=Multistability and critical thresholds of the Greenland ice sheet |journal=Nature Climate Change |date=11 March 2012 |volume=2 |issue=6 |pages=429–432 |doi=10.1038/nclimate1449 |bibcode=2012NatCC...2..429R}}</ref> 2023 modelling has narrowed the tipping threshold to a {{convert|1.7|C-change|F-change}}-{{convert|2.3|C-change|F-change}} range. If temperatures reach or exceed that level, reducing the global temperature to {{convert|1.5|C-change|F-change}} above pre-industrial levels or lower would prevent the loss of the entire ice sheet. One way to do this in theory would be large-scale [[carbon dioxide removal]]. But it would also cause greater losses and sea level rise from Greenland than if the threshold was not breached in the first place.<ref name="Bochow2023">{{cite journal |last1=Bochow |first1=Nils |last2=Poltronieri |first2=Anna |last3=Robinson |first3=Alexander |last4=Montoya |first4=Marisa |last5=Rypdal |first5=Martin |last6=Boers |first6=Niklas |date=18 October 2023 |title=Overshooting the critical threshold for the Greenland ice sheet |journal=Nature |volume=622 |issue=7983 |pages=528–536 |bibcode=2023Natur.622..528B |doi=10.1038/s41586-023-06503-9 |pmc=10584691 |pmid=37853149}}</ref> Otherwise, the ice sheet would take between 10,000 and 15,000 years to disintegrate entirely once the tipping point had been crossed. The most likely estimate is 10,000 years.<ref name="ArmstrongMcKay2022" /><ref name="ArmstrongMcKayExplainer" /> If climate change continues along its worst trajectory and temperatures continue to rise quickly over multiple centuries, it would only take 1,000 years.<ref name="Aschwanden2019">{{Cite journal |last1=Aschwanden |first1=Andy |last2=Fahnestock |first2=Mark A. |last3=Truffer |first3=Martin |last4=Brinkerhoff |first4=Douglas J. |last5=Hock |first5=Regine |last6=Khroulev |first6=Constantine |last7=Mottram |first7=Ruth |last8=Khan |first8=S. Abbas |date=19 June 2019 |title=Contribution of the Greenland Ice Sheet to sea level over the next millennium |journal=Science Advances |volume=5 |issue=6 |pages=218–222 |language=EN |doi=10.1126/sciadv.aav9396 |pmid=31223652 |pmc=6584365 |bibcode=2019SciA....5.9396A}}</ref>

===Mountain glacier loss===
[[File:2015-2100 Impacts of global warming on glaciers and sea level rise.svg|thumb|upright=1.2|Based on national pledges to reduce greenhouse gas emissions, global mean temperature is projected to increase by {{convert|2.7|C-change|F-change}}, which would cause loss of about half of Earth's glaciers by 2100—causing a sea level rise of 115±40 millimeters.<ref name=Science_20230105>{{cite journal |last1=Rounce |first1=David R. |last2=Hock |first2=Regine |last3=Maussion |first3=Fabien |last4=Hugonnet |first4=Romain |last5=Kochtitzky |first5=William |last6=Huss |first6=Matthias |last7=Berthier |first7=Etienne |last8=Brinkerhoff |first8=Douglas |last9=Compagno |first9=Loris |last10=Copland |first10=Luke |last11=Farinotti |first11=Daniel |last12=Menounos |first12=Brian |last13=McNabb |first13=Robert W. |display-authors=4 |title=Global glacier change in the 21st century: Every increase in temperature matters |journal=Science |date=5 January 2023 |volume=379 |issue=6627 |pages=78–83 |doi=10.1126/science.abo1324 |pmid=36603094 |bibcode=2023Sci...379...78R |s2cid=255441012 |url=https://www.science.org/doi/10.1126/science.abo1324}}</ref>]]

There are roughly 200,000 glaciers on Earth, which are spread out across all continents.<ref name="Huss-2015">{{cite journal |last1=Huss |first1=Matthias |last2=Hock |first2=Regine |title=A new model for global glacier change and sea-level rise |journal=Frontiers in Earth Science |date=30 September 2015 |volume=3 |page=54 |doi=10.3389/feart.2015.00054 |bibcode=2015FrEaS...3...54H |s2cid=3256381 |doi-access=free}}</ref> Less than 1% of glacier ice is in mountain glaciers, compared to 99% in Greenland and [[Antarctica]]. However, this small size also makes mountain glaciers more vulnerable to melting than the larger ice sheets. This means they have had a disproportionate contribution to historical sea level rise and are set to contribute a smaller, but still significant fraction of sea level rise in the 21st century.<ref>{{cite journal |last1=Radić |first1=Valentina |last2=Hock |first2=Regine |title=Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise |journal=Nature Geoscience |date=9 January 2011 |volume=4 |issue=2 |pages=91–94 |doi=10.1038/ngeo1052 |bibcode=2011NatGe...4...91R}}</ref> Observational and modelling studies of [[Retreat of glaciers since 1850|mass loss from glaciers and ice caps]] show they contribute 0.2-0.4&nbsp;mm per year to sea level rise, averaged over the 20th century.<ref>{{cite report |doi=10.7265/N52N506F |year=2002 |last1=Dyurgerov |first1=Mark |title=Glacier Mass Balance and Regime Measurements and Analysis, 1945-2003}}</ref> The contribution for the 2012–2016 period was nearly as large as that of Greenland. It was 0.63&nbsp;mm of sea level rise per year, equivalent to 34% of sea level rise from ''land ice'' sources.<ref name="Bamber2018" /> Glaciers contributed around 40% to sea level rise during the 20th century, with estimates for the 21st century of around 30%.<ref name="WCRP2018"/>

In 2023, a ''[[Science (magazine)|Science]]'' paper estimated that at {{convert|1.5|C-change|F-change}}, one quarter of mountain glacier mass would be lost by 2100 and nearly half would be lost at {{convert|4|C-change|F-change}}, contributing ~{{cvt|9|cm|in|frac=2}} and ~{{cvt|15|cm|in|frac=2}} to sea level rise, respectively. Glacier mass is disproportionately concentrated in the most resilient glaciers. So in practice this would remove 49-83% of glacier formations. It further estimated that the current likely trajectory of {{convert|2.7|C-change|F-change}} would result in the SLR contribution of ~{{cvt|11|cm|in|frac=2}} by 2100.<ref>{{Cite journal |last1=Rounce |first1=David R. |last2=Hock |first2=Regine |last3=Maussion |first3=Fabien |last4=Hugonnet |first4=Romain |last5=Kochtitzky |first5=William |last6=Huss |first6=Matthias |last7=Berthier|first7=Etienne |last8=Brinkerhoff |first8=Douglas |last9=Compagno |first9=Loris |last10=Copland |first10=Luke |last11=Farinotti |first11=Daniel |last12=Menounos |first12=Brian |last13=McNabb |first13=Robert W. |date=5 January 2023 |title=Global glacier change in the 21st century: Every increase in temperature matters |url=https://www.science.org/doi/10.1126/science.abo1324 |journal=Science |language=en |volume=79 |issue=6627 |pages=78–83 |doi=10.1126/science.abo1324 |pmid=36603094 |bibcode=2023Sci...379...78R |s2cid=255441012}}</ref> Mountain glaciers are even more vulnerable over the longer term. In 2022, another ''Science'' paper estimated that almost no mountain glaciers could survive once warming crosses {{convert|2|C-change|F-change}}. Their complete loss is largely inevitable around {{convert|3|C-change|F-change}}. There is even a possibility of complete loss after 2100 at just {{convert|1.5|C-change|F-change}}. This could happen as early as 50 years after the tipping point is crossed, although 200 years is the most likely value, and the maximum is around 1000 years.<ref name="ArmstrongMcKay2022" /><ref name="ArmstrongMcKayExplainer" />

=== Sea ice loss ===
Sea ice loss contributes very slightly to global sea level rise. If the melt water from ice floating in the sea was exactly the same as sea water then, according to [[Archimedes' principle]], no rise would occur. However melted sea ice contains less [[salinity|dissolved salt]] than sea water and is therefore less [[density|dense]], with a slightly greater volume per unit of mass. If all floating [[ice shelf|ice shelves]] and [[icebergs]] were to melt sea level would only rise by about {{convert|4|cm|in|frac=2|abbr=on}}.<ref>{{cite journal |last1=Noerdlinger |first1=Peter D. |last2=Brower |first2=Kay R. |title=The melting of floating ice raises the ocean level |journal=Geophysical Journal International |date=July 2007 |volume=170 |issue=1 |pages=145–150 |doi=10.1111/j.1365-246X.2007.03472.x |bibcode=2007GeoJI.170..145N |doi-access=free}}</ref>
[[File:Trends-in-land-water-storage-from-GRACE-observations,-April-2002-to-November-2014.jpg|thumb|upright=1.6|right|Trends in land water storage from [[Gravity Recovery and Climate Experiment|GRACE]] observations in gigatons per year, April 2002 to November 2014 (glaciers and ice sheets are excluded).]]

=== Changes to land water storage ===
{{See also|Groundwater-related subsidence|}}

Human activity impacts how much water is stored on land. [[Dam]]s retain large quantities of water, which is stored on land rather than flowing into the sea, though the total quantity stored will vary from time to time. On the other hand, humans extract water from lakes, [[wetland]]s and [[Aquifer|underground reservoirs]] for drinking and [[Food industry|food production]]. This often causes [[subsidence]]. Furthermore, the [[Water cycle|hydrological cycle]] is influenced by climate change and [[deforestation]]. In the 20th century, these processes had approximately cancelled out each other's impact on sea level rise, but dam building has slowed down and is expected to stay low for the 21st century.<ref>{{cite journal |last1=Wada |first1=Yoshihide |last2=Reager |first2=John T. |last3=Chao |first3=Benjamin F. |last4=Wang |first4=Jida |last5=Lo |first5=Min-Hui |last6=Song |first6=Chunqiao |last7=Li |first7=Yuwen |last8=Gardner |first8=Alex S. |title=Recent Changes in Land Water Storage and its Contribution to Sea Level Variations |journal=Surveys in Geophysics |date=15 November 2016 |volume=38 |issue=1 |pages=131–152 |doi=10.1007/s10712-016-9399-6 |pmid=32269399 |pmc=7115037}}</ref><ref name="ipcc13" />{{rp|1155}}

Water redistribution caused by [[irrigation]] from 1993 to 2010 caused a drift of Earth's [[Geographical pole|rotational pole]] by {{convert|78.48|cm|in}}. This caused groundwater depletion equivalent to a global sea level rise of {{convert|6.24|mm|inches}}.<ref name=GeophysRschLtrs_20230615>{{cite journal |last1=Seo |first1=Ki-Weon |last2=Ryu |first2=Dongryeol |last3=Eom |first3=Jooyoung |last4=Jeon |first4=Taewhan |last5=Kim |first5=Jae-Seung |last6=Youm |first6=Kookhyoun |last7=Chen |first7=Jianli |last8=Wilson |first8=Clark R. |title=Drift of Earth's Pole Confirms Groundwater Depletion as a Significant Contributor to Global Sea Level Rise 1993–2010 |journal=Geophysical Research Letters |date=15 June 2023 |volume=50 |issue=12 |page=e2023GL103509 |doi=10.1029/2023GL103509 |bibcode=2023GeoRL..5003509S |s2cid=259275991 |url=https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GL103509}}</ref>

== Impacts ==
{{see also|Coast#Human impacts|l1=Human impacts on coasts|Coastal development hazards|l2=|Coastal erosion|||}}

=== On people and societies ===
[[File:1950- High tide flooding, by year - NOAA tide gauges (U.S.).svg|thumb|left|High tide flooding, also called tidal flooding, has become much more common in the past seven decades.<ref name="N0AAHighTideFlooding201802">{{cite web |last1=Sweet |first1=William V. |last2=Dusek |first2=Greg |last3=Obeysekera |first3=Jayantha |last4=Marra |first4=John J. |title=Patterns and Projections of High Tide Flooding Along the U.S. Coastline Using a Common Impact Threshold |url=https://tidesandcurrents.noaa.gov/publications/techrpt86_PaP_of_HTFlooding.pdf |website=tidesandcurrents.NOAA.gov |publisher=National Oceanic and Atmospheric Administration (NOAA) |archive-url=https://web.archive.org/web/20221015221519/https://tidesandcurrents.noaa.gov/publications/techrpt86_PaP_of_HTFlooding.pdf |archive-date=15 October 2022 |page=4 |date=February 2018 |quote=Fig. 2b |url-status=live}}</ref>]]
Sea-level rise has many impacts. They include higher and more frequent high-tide and [[storm surge|storm-surge]] flooding and increased [[coastal erosion]]. Other impacts are inhibition of [[primary production]] processes, more extensive coastal inundation, and changes in surface [[water quality]] and [[groundwater]]. These can lead to a greater loss of property and coastal habitats, loss of life during floods and loss of cultural resources. There are also impacts on agriculture and [[aquaculture]]. There can also be loss of tourism, recreation, and transport-related functions.<ref name="IPCC-2001">{{Cite report|url=https://www.ipcc.ch/site/assets/uploads/2018/03/WGI_TAR_full_report.pdf|title=TAR Climate Change 2001: The Scientific Basis|date=2001|publisher=International Panel on Climate Change, Cambridge University Press|isbn=0521-80767-0|access-date=23 July 2021}}</ref>{{rp|356}} [[Land use]] changes such as [[urbanisation]] or [[deforestation]] of low-lying coastal zones exacerbate coastal flooding impacts. Regions already vulnerable to rising sea level also struggle with coastal flooding. This washes away land and alters the landscape.<ref>{{Cite journal|last=Wu|first=Tao|date=October 2021|title=Quantifying coastal flood vulnerability for climate adaptation policy using principal component analysis|url=https://linkinghub.elsevier.com/retrieve/pii/S1470160X21006713|journal=Ecological Indicators|language=en|volume=129|page=108006|doi=10.1016/j.ecolind.2021.108006|bibcode=2021EcInd.12908006W}}</ref>

Changes in emissions are likely to have only a small effect on the extent of sea level rise by 2050.<ref name="us nrc 2011 long term slr" /> So projected sea level rise could put tens of millions of people at risk by then. Scientists estimate that 2050 levels of sea level rise would result in about 150 million people under the water line during high tide. About 300 million would be in places flooded every year. This projection is based on the distribution of population in 2010. It does not take into account the effects of [[population growth]] and [[human migration]]. These figures are 40 million and 50 million more respectively than the numbers at risk in 2010.<ref name="Kulp2019">{{cite journal |last1=Kulp |first1=Scott A. |last2=Strauss |first2=Benjamin H. |title=New elevation data triple estimates of global vulnerability to sea-level rise and coastal flooding |journal=Nature Communications |date=29 October 2019 |volume=10 |issue=1 |page=4844 |doi=10.1038/s41467-019-12808-z |pmid=31664024 |pmc=6820795 |bibcode=2019NatCo..10.4844K}}</ref><ref>{{cite news|url=https://www.ecowatch.com/sea-level-rise-predictions-2641159739.html|title=300 Million People Worldwide Could Suffer Yearly Flooding by 2050|last1=Rosane|first1=Olivia|date=October 30, 2019|access-date=31 October 2019|agency=Ecowatch}}</ref> By 2100, there would be another 40 million people under the water line during high tide if sea level rise remains low. This figure would be 80 million for a high estimate of median sea level rise.<ref name="Kulp2019" /> Ice sheet processes under the highest [[Climate change scenario|emission scenario]] would result in sea level rise of well over {{convert|1|m|ft|frac=4|spell=in}} by 2100. This could be as much as over {{convert|2|m|ft|frac=2|spell=in}},<ref name="NOAA-2022" /><ref name="IPCC_2021_WGI_SPM" />{{rp|TS-45}} This could result in as many as 520 million additional people ending up under the water line during high tide and 640&nbsp;million in places flooded every year, compared to the 2010 population distribution.<ref name="Kulp2019" />
[[File:Major cities threatened by sea level rise.png|thumb|upright=1.35|Major cities threatened by sea level rise of {{cvt|49|cm|ft|frac=2}} compared to the level in 2010.]]
Over the longer term, coastal areas are particularly vulnerable to rising sea levels. They are also vulnerable to changes in the frequency and intensity of storms, increased precipitation, and rising [[ocean temperature]]s. Ten percent of the world's population live in coastal areas that are less than {{Convert|10|m|ft}} above sea level. Two thirds of the world's cities with over five million people are located in these low-lying coastal areas.<ref>{{cite journal |last1=McGranahan |first1=Gordon |last2=Balk |first2=Deborah |last3=Anderson |first3=Bridget |title=The rising tide: assessing the risks of climate change and human settlements in low elevation coastal zones |journal=Environment and Urbanization |date=29 June 2016 |volume=19 |issue=1 |pages=17–37 |doi=10.1177/0956247807076960 |s2cid=154588933}}</ref> About 600 million people live directly on the coast around the world.<ref>{{cite news |last1=Sengupta |first1=Somini |others=Photographer: Chang W. Lee|title=A Crisis Right Now: San Francisco and Manila Face Rising Seas |url=https://www.nytimes.com/interactive/2020/02/13/climate/manila-san-francisco-sea-level-rise.html |access-date=4 March 2020 |work=The New York Times |date=13 February 2020}}</ref> Cities such as [[Miami]], [[Rio de Janeiro]], [[Osaka]] and [[Shanghai]] will be especially vulnerable later in the century under warming of 3&nbsp;°C (5.4&nbsp;°F). This is close to the current trajectory.<ref name="Holder-2017">{{Cite news|last1=Holder|first1=Josh|last2=Kommenda|first2=Niko|last3=Watts|first3=Jonathan|date=3 November 2017|title=The three-degree world: cities that will be drowned by global warming|work=The Guardian|url=https://www.theguardian.com/cities/ng-interactive/2017/nov/03/three-degree-world-cities-drowned-global-warming|access-date=2018-12-28}}</ref><ref name="CAT" /> [[Lidar|LiDAR]]-based research had established in 2021 that 267 million people worldwide lived on land less than {{cvt|2|m|ft|frac=2}} above sea level. With a {{cvt|1|m|ft|frac=2}} sea level rise and zero population growth, that could increase to 410 million people.<ref>{{Cite web|last=Storer|first=Rhi|date=2021-06-29|title=Up to 410 million people at risk from sea level rises – study|url=http://www.theguardian.com/environment/2021/jun/29/risk-from-sea-level-rises-unless-emissions-reduced|access-date=2021-07-01|website=The Guardian|language=en}}</ref><ref>{{Cite journal|last1=Hooijer|first1=A.|last2=Vernimmen|first2=R.|date=2021-06-29|title=Global LiDAR land elevation data reveal greatest sea-level rise vulnerability in the tropics|journal=Nature Communications|language=en|volume=12|issue=1|page=3592|doi=10.1038/s41467-021-23810-9|pmid=34188026|pmc=8242013|bibcode=2021NatCo..12.3592H|issn=2041-1723}}</ref>

Potential disruption of sea trade and migrations could impact people living further inland. United Nations Secretary-General [[António Guterres]] warned in 2023 that sea level rise risks causing [[Climate migrant|human migrations]] on a "biblical scale".<ref>{{Cite news|last1=Carrington|first1=Damian|date=14 February 2023|title=Rising seas threaten 'mass exodus on a biblical scale', UN chief warns|work=The Guardian|url=https://www.theguardian.com/environment/2023/feb/14/rising-seas-threaten-mass-exodus-on-a-biblical-scale-un-chief-warns|access-date=2023-02-25}}</ref> Sea level rise will inevitably affect [[port]]s, but there is limited research on this. There is insufficient knowledge about the investments necessary to protect ports currently in use. This includes protecting current facilities before it becomes more reasonable to build new ports elsewhere.<ref>{{Cite journal|last1=Xia|first1=Wenyi|last2=Lindsey|first2=Robin|date=October 2021|title=Port adaptation to climate change and capacity investments under uncertainty|url=https://linkinghub.elsevier.com/retrieve/pii/S0191261521001600|journal=Transportation Research Part B: Methodological|language=en|volume=152|pages=180–204|doi=10.1016/j.trb.2021.08.009|bibcode=2021TRPB..152..180X |s2cid=239647501}}</ref><ref>{{Cite web|title=Chapter 4: Sea Level Rise and Implications for Low-Lying Islands, Coasts and Communities — Special Report on the Ocean and Cryosphere in a Changing Climate|url=https://www.ipcc.ch/srocc/chapter/chapter-4-sea-level-rise-and-implications-for-low-lying-islands-coasts-and-communities/|access-date=2021-12-17}}</ref> Some coastal regions are rich agricultural lands. Their loss to the sea could cause [[food insecurity|food shortage]]s. This is a particularly acute issue for [[river delta]]s such as [[Nile Delta]] in [[Egypt]] and [[Red River Delta|Red River]] and [[Mekong Delta]]s in Vietnam. Saltwater intrusion into the soil and [[irrigation]] water has a disproportionate effect on them.<ref name="Michaelson-2018" /><ref name="Nagothu-2017">{{Cite web |last=Nagothu |first=Udaya Sekhar |date=2017-01-18 |title=Food security threatened by sea-level rise |url=https://www.nibio.no/nyheter/food-security-threatened-by-sea-level-rise |access-date=2018-10-21 |publisher=Nibio}}</ref>

===On ecosystems===
{{See also|Extinction risk from climate change}}
[[File:Bramble-cay-melomys.jpg|thumb|left|[[Bramble Cay melomys]], the first known mammal species to go extinct due to sea level rise.]]
Flooding and soil/water salinization threaten the habitats of [[coast]]al plants, birds, and freshwater/[[estuarine]] fish when seawater reaches inland.<ref name="National Geographic-2017">{{Cite web|url=https://www.nationalgeographic.com/environment/global-warming/sea-level-rise/|archive-url=https://web.archive.org/web/20170117004107/http://www.nationalgeographic.com/environment/global-warming/sea-level-rise/|archive-date=January 17, 2017|title=Sea Level Rise|date=January 13, 2017|website=National Geographic}}</ref> When coastal [[forest]] areas become inundated with saltwater to the point no trees can survive the resulting habitats are called [[ghost forest]]s.<ref>{{cite web|url=http://grist.org/article/ghost-forests-are-eerie-evidence-of-rising-seas/|title=Ghost forests are eerie evidence of rising seas|date=18 September 2016|website=Grist.org|access-date=2017-05-17}}</ref><ref>{{cite web|url=http://e360.yale.edu/features/ghost_forest_rising_sea_levels_killing_coastal_woodlands|title=How Rising Seas Are Killing Southern U.S. Woodlands - Yale E360|website=e360.yale.edu|access-date=2017-05-17}}</ref> Starting around 2050, some nesting sites in [[Florida]], [[Cuba]], [[Ecuador]] and the island of [[Sint Eustatius]] for [[leatherback turtle|leatherback]], [[loggerhead turtle|loggerhead]], [[hawksbill turtle|hawksbill]], [[green turtle|green]] and [[olive ridley turtle]]s are expected to be flooded. The proportion will increase over time.<ref>{{Cite journal |last1=Rivas |first1=Marga L. |last2=Rodríguez-Caballero |first2=Emilio |last3=Esteban |first3=Nicole |last4=Carpio |first4=Antonio J. |last5=Barrera-Vilarmau |first5=Barbara |last6=Fuentes |first6=Mariana M. P. B. |last7=Robertson |first7=Katharine |last8=Azanza |first8=Julia |last9=León |first9=Yolanda |last10=Ortega |first10=Zaida |date=2023-04-20 |title=Uncertain future for global sea turtle populations in face of sea level rise |journal=Scientific Reports |language=en |volume=13 |issue=1 |page=5277 |doi=10.1038/s41598-023-31467-1 |pmid=37081050 |pmc=10119306 |bibcode=2023NatSR..13.5277R |issn=2045-2322}}</ref> In 2016, [[Bramble Cay]] islet in the [[Great Barrier Reef]] was inundated. This flooded the habitat of a rodent named [[Bramble Cay melomys]].<ref>{{cite web|url=http://www.australiangeographic.com.au/news/2016/06/extinct-bramble-cay-melomys|title=Extinct: Bramble Cay melomys|last=Smith|first=Lauren|date=2016-06-15|website=Australian Geographic|access-date=2016-06-17}}</ref> It was officially declared extinct in 2019.<ref>{{Cite web|url=https://www.smh.com.au/environment/climate-change/our-little-brown-rat-first-climate-change-caused-mammal-extinction-20190219-p50yry.html|title='Our little brown rat': first climate change-caused mammal extinction|last=Hannam|first=Peter|date=2019-02-19|website=The Sydney Morning Herald|language=en|access-date=2019-06-25}}</ref>
[[File:Mangroves.jpg|thumb|An example of mangrove pneumatophores.]]
Some ecosystems can move inland with the high-water mark. But natural or artificial barriers prevent many from migrating. This coastal narrowing is sometimes called 'coastal squeeze' when it involves human-made barriers. It could result in the loss of habitats such as [[mudflat]]s and [[tidal marsh]]es.<ref name="birdlife-2015">{{Cite web|url=http://datazone.birdlife.org/sea-level-rise-poses-a-major-threat-to-coastal-ecosystems-and-the-biota-they-support|title=Sea level rise poses a major threat to coastal ecosystems and the biota they support|date=2015|website=birdlife.org|publisher=Birdlife International}}</ref><ref>{{cite journal |last1=Pontee |first1=Nigel |title=Defining coastal squeeze: A discussion |journal=Ocean & Coastal Management |date=November 2013 |volume=84 |pages=204–207 |doi=10.1016/j.ocecoaman.2013.07.010 |bibcode=2013OCM....84..204P}}</ref> [[Mangrove]] ecosystems on the mudflats of tropical coasts nurture high [[biodiversity]]. They are particularly vulnerable due to mangrove plants' reliance on breathing roots or [[pneumatophores]]. These will be submerged if the rate is too rapid for them to migrate upward. This would result in the loss of an ecosystem.<ref>{{Cite web|url=https://www.nrc.govt.nz/for-schools/school-information-packs/mangroves/|title=Mangroves - Northland Regional Council|website=www.nrc.govt.nz}}</ref><ref name="High mangrove density enhances surf">{{cite journal |last1=Kumara |first1=M. P. |last2=Jayatissa |first2=L. P. |last3=Krauss |first3=K. W. |last4=Phillips |first4=D. H. |last5=Huxham |first5=M. |title=High mangrove density enhances surface accretion, surface elevation change, and tree survival in coastal areas susceptible to sea-level rise |journal=Oecologia |pages=545–553 |date=2010|volume=164 |issue=2 |doi=10.1007/s00442-010-1705-2 |jstor=40864709 |pmid=20593198 |bibcode=2010Oecol.164..545K |s2cid=6929383}}</ref><ref>{{cite journal |last1=Krauss |first1=Ken W. |last2=McKee |first2=Karen L. |last3=Lovelock |first3=Catherine E. |last4=Cahoon |first4=Donald R. |last5=Saintilan |first5=Neil |last6=Reef |first6=Ruth |last7=Chen |first7=Luzhen |title=How mangrove forests adjust to rising sea level |journal=New Phytologist |date=April 2014 |volume=202 |issue=1 |pages=19–34 |doi=10.1111/nph.12605 |pmid=24251960 |url=https://digitalcommons.unl.edu/usgsstaffpub/986}}</ref><ref name="A Conceptual Model for the Response">{{cite journal|last1=Soares|first1=M.L.G.|date=2009|title=A Conceptual Model for the Responses of Mangrove Forests to Sea Level Rise|journal=Journal of Coastal Research|pages=267–271|jstor=25737579}}</ref> Both mangroves and [[tidal marsh]]es protect against storm surges, waves and tsunamis, so their loss makes the effects of sea level rise worse.<ref>{{cite journal |last1=Crosby |first1=Sarah C. |last2=Sax |first2=Dov F. |last3=Palmer |first3=Megan E. |last4=Booth |first4=Harriet S. |last5=Deegan |first5=Linda A. |last6=Bertness |first6=Mark D. |last7=Leslie |first7=Heather M. |title=Salt marsh persistence is threatened by predicted sea-level rise |journal=Estuarine, Coastal and Shelf Science |date=November 2016 |volume=181 |pages=93–99 |doi=10.1016/j.ecss.2016.08.018 |bibcode=2016ECSS..181...93C |doi-access=free}}</ref><ref>{{cite web|url=https://www.nature.org/media/oceansandcoasts/mangroves-for-coastal-defence.pdf|title=Mangroves for coastal defence. Guidelines for coastal managers & policy makers|author1=Spalding, M.|author2=McIvor, A.|date=2014|publisher=[[Wetlands International]] and [[The Nature Conservancy]]|author3=Tonneijck, F.H.|author4=Tol, S.|author5=van Eijk, P.}}</ref> Human activities such as dam building may restrict sediment supplies to wetlands. This would prevent natural adaptation processes. The loss of some tidal marshes is unavoidable as a consequence.<ref>{{cite journal |last1=Weston |first1=Nathaniel B. |title=Declining Sediments and Rising Seas: an Unfortunate Convergence for Tidal Wetlands |journal=Estuaries and Coasts |date=16 July 2013 |volume=37 |issue=1 |pages=1–23 |doi=10.1007/s12237-013-9654-8 |s2cid=128615335}}</ref>

[[Coral]]s are important for bird and fish life. They need to grow vertically to remain close to the sea surface in order to get enough energy from sunlight. The corals have so far been able to keep up the vertical growth with the rising seas, but might not be able to do so in the future.<ref>{{Cite book|title=Climate Change 2014: Impacts, Adaptation, and Vulnerability.|last1=Wong|first1=Poh Poh|last2=Losado|first2=I.J.|last3=Gattuso|first3=J.-P.|last4=Hinkel|first4=Jochen|publisher=Cambridge University Press|year=2014|location=New York|chapter=Coastal Systems and Low-Lying Areas|chapter-url=http://www.ipcc.ch/pdf/assessment-report/ar5/wg2/WGIIAR5-Chap5_FINAL.pdf|access-date=2018-10-07|archive-date=2018-11-23|archive-url=https://web.archive.org/web/20181123125554/http://www.ipcc.ch/pdf/assessment-report/ar5/wg2/WGIIAR5-Chap5_FINAL.pdf}}</ref>

== Adaptation ==
{{further|Climate change adaptation|coastal management}}
[[File:Oosterscheldekering-pohled.jpg|thumb|left|[[Oosterscheldekering]], the largest barrier of the Dutch [[Delta Works]].]]
[[Climate change mitigation|Cutting greenhouse gas emissions]] can slow and stabilize the rate of sea level rise after 2050. This would greatly reduce its costs and damages, but cannot stop it outright. So [[climate change adaptation]] to sea level rise is inevitable.<ref>Cooley, S., D. Schoeman, L. Bopp, P. Boyd, S. Donner, D.Y. Ghebrehiwet, S.-I. Ito, W. Kiessling, P. Martinetto, E. Ojea, M.-F. Racault, B. Rost, and M. Skern-Mauritzen, 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_FinalDraft_Chapter03.pdf Ocean and Coastal Ecosystems and their Services (Chapter 3)]. In: ''Climate Change 2022: Impacts, Adaptation, and Vulnerability.'' Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [H.-O. Pörtner, D.C. Roberts, M. Tignor, E.S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press. In Press. - Cross-Chapter Box SLR: Sea Level Rise</ref>{{rp||page=3–127}} The simplest approach is to stop development in vulnerable areas and ultimately move people and [[infrastructure]] away from them. Such ''retreat'' from sea level rise often results in the loss of livelihoods. The displacement of newly impoverished people could burden their new homes and accelerate social tensions.<ref>{{Cite journal |last1=Dasgupta |first1=Susmita |last2=Wheeler |first2=David |last3=Bandyopadhyay |first3=Sunando |last4=Ghosh |first4=Santadas |last5=Roy |first5=Utpal |date=February 2022 |title=Coastal dilemma: Climate change, public assistance and population displacement |url=https://linkinghub.elsevier.com/retrieve/pii/S0305750X21003223 |journal=World Development |language=en |volume=150 |page=105707 |doi=10.1016/j.worlddev.2021.105707 |issn=0305-750X |s2cid=244585347}}</ref>

It is possible to avoid or at least delay the ''retreat'' from sea level rise with enhanced ''protections.'' These include [[dam]]s, [[levee]]s or improved natural defenses.<ref name="Thomsen-2012" /> Other options include updating [[Building code|building standards]] to reduce damage from floods, addition of storm water valves to address more frequent and severe flooding at high tide,<ref name="US EPA">{{cite web |date=2 May 2016 |title=Climate Adaptation and Sea Level Rise |url=https://www.epa.gov/arc-x/climate-adaptation-and-sea-level-rise |website=US EPA, Climate Change Adaptation Resource Center (ARC-X) |language=en}}</ref> or cultivating crops more tolerant of saltwater in the soil, even at an increased cost.<ref name="Nagothu-2017" /><ref name="Thomsen-2012" /><ref name="Fletcher-2013">{{cite journal |last1=Fletcher |first1=Cameron |date=2013 |title=Costs and coasts: an empirical assessment of physical and institutional climate adaptation pathways |url=https://apo.org.au/node/34006 |journal=Apo}}</ref> These options divide into ''hard'' and ''soft'' adaptation. Hard adaptation generally involves large-scale changes to human societies and ecological systems. It often includes the construction of capital-intensive infrastructure. Soft adaptation involves strengthening [[nature-based solutions|natural defenses]] and local community adaptation. This usually involves simple, modular and locally owned technology. The two types of adaptation may be complementary or mutually exclusive.<ref name="Fletcher-2013" /><ref>{{Cite journal |last=Sovacool |first=Benjamin K. |date=2011 |title=Hard and soft paths for climate change adaptation |url=http://www.adaptation-undp.org/sites/default/files/downloads/sovacool-cp-hardsoft.pdf |url-status=dead |journal=Climate Policy |volume=11 |issue=4 |pages=1177–1183 |bibcode=2011CliPo..11.1177S |doi=10.1080/14693062.2011.579315 |s2cid=153384574 |archive-url=https://web.archive.org/web/20200710010054/https://www.adaptation-undp.org/sites/default/files/downloads/sovacool-cp-hardsoft.pdf |archive-date=2020-07-10 |access-date=2018-09-02}}</ref> Adaptation options often require significant investment. But the costs of doing nothing are far greater. One example would involve adaptation against flooding. Effective adaptation measures could reduce future annual costs of flooding in 136 of the world's largest coastal cities from $1 trillion by 2050 without adaptation to a little over $60 billion annually. The cost would be $50 billion per year.<ref>{{cite web |date=18 August 2013 |title=Coastal cities face rising risk of flood losses, study says |url=https://phys.org/news/2013-08-coastal-cities-losses.html |access-date=17 April 2023 |publisher=Phys.org}}</ref><ref>{{cite journal |last1=Hallegatte |first1=Stephane |last2=Green |first2=Colin |last3=Nicholls |first3=Robert J. |last4=Corfee-Morlot |first4=Jan |date=18 August 2013 |title=Future flood losses in major coastal cities |url=https://www.nature.com/articles/nclimate1979 |journal=Nature Climate Change |language=en |volume=3 |issue=9 |pages=802–806 |bibcode=2013NatCC...3..802H |doi=10.1038/nclimate1979}}</ref> Some experts argue that retreat from the coast would have a lower impact on the [[GDP]] of [[India]] and [[Southeast Asia]] then attempting to protect every coastline, in the case of very high sea level rise.<ref>{{cite journal |last1=Bachner |first1=Gabriel |last2=Lincke |first2=Daniel |last3=Hinkel |first3=Jochen |date=29 September 2022 |title=The macroeconomic effects of adapting to high-end sea-level rise via protection and migration |journal=Nature Communications |language=en |volume=13 |issue=1 |page=5705 |bibcode=2022NatCo..13.5705B |doi=10.1038/s41467-022-33043-z |pmc=9522673 |pmid=36175422}}</ref> 
[[File:Hurk_2022_UK_SLR_adaptation.jpg|thumb|upright=1.4|Planning for the future sea level rise used in the [[United Kingdom]].<ref name="Hurk2022" />]]
To be successful, adaptation must anticipate sea level rise well ahead of time. As of 2023, the global state of adaptation planning is mixed. A survey of 253 planners from 49 countries found that 98% are aware of sea level rise projections, but 26% have not yet formally integrated them into their policy documents. Only around a third of respondents from Asian and South American countries have done so. This compares with 50% in Africa, and over 75% in Europe, Australasia and North America. Some 56% of all surveyed planners have plans which account for 2050 and 2100 sea level rise. But 53% use only a single projection rather than a range of two or three projections. Just 14% use four projections, including the one for "extreme" or "high-end" sea level rise.<ref>{{cite journal |last1=Hirschfeld |first1=Daniella |last2=Behar |first2=David |last3=Nicholls |first3=Robert J. |last4=Cahill |first4=Niamh |last5=James |first5=Thomas |last6=Horton |first6=Benjamin P. |last7=Portman |first7=Michelle E. |last8=Bell |first8=Rob |last9=Campo |first9=Matthew |last10=Esteban |first10=Miguel |last11=Goble |first11=Bronwyn |last12=Rahman |first12=Munsur |last13=Appeaning Addo |first13=Kwasi |last14=Chundeli |first14=Faiz Ahmed |last15=Aunger |first15=Monique |date=3 April 2023 |title=Global survey shows planners use widely varying sea-level rise projections for coastal adaptation |journal=Communications Earth & Environment |language=en |volume=4 |issue=1 |page=102 |bibcode=2023ComEE...4..102H |doi=10.1038/s43247-023-00703-x |doi-access=free |last16=Babitsky |first16=Orly |last17=Beal |first17=Anders |last18=Boyle |first18=Ray |last19=Fang |first19=Jiayi |last20=Gohar |first20=Amir |last21=Hanson |first21=Susan |last22=Karamesines |first22=Saul |last23=Kim |first23=M. J. |last24=Lohmann |first24=Hilary |last25=McInnes |first25=Kathy |last26=Mimura |first26=Nobuo |last27=Ramsay |first27=Doug |last28=Wenger |first28=Landis |last29=Yokoki |first29=Hiromune|pmid=38665203 |pmc=11041751}} [[File:CC-BY_icon.svg|50x50px]] Text and images are available under a [[creativecommons:by/4.0/|Creative Commons Attribution 4.0 International License]].</ref> Another study found that over 75% of regional sea level rise assessments from the [[West Coast of the United States|West]] and [[Northeastern United States]] included at least three estimates. These are usually [[Representative Concentration Pathway|RCP2.6]], RCP4.5 and RCP8.5, and sometimes include extreme scenarios. But 88% of projections from the [[American South]] had only a single estimate. Similarly, no assessment from the South went beyond 2100. By contrast 14 assessments from the West went up to 2150, and three from the Northeast went to 2200. 56% of all localities were also found to underestimate the upper end of sea level rise relative to [[IPCC Sixth Assessment Report]].<ref>{{cite journal |last1=Garner |first1=Andra J. |last2=Sosa |first2=Sarah E. |last3=Tan |first3=Fangyi |last4=Tan |first4=Christabel Wan Jie |last5=Garner |first5=Gregory G. |last6=Horton |first6=Benjamin P. |date=23 January 2023 |title=Evaluating Knowledge Gaps in Sea-Level Rise Assessments From the United States |url=https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022EF003187 |journal=Earth's Future |volume=11 |issue=2 |pages=e2022EF003187 |bibcode=2023EaFut..1103187G |doi=10.1029/2022EF003187 |s2cid=256227421}}</ref>

== By region ==
=== Africa ===
{{Further|Climate change in the Middle East and North Africa#Sea level rise}}

[[File:ANKOMAH 20221122-009.jpg|thumb|A man looking out over the beach from a building destroyed by high tides in [[Chorkor]], a suburb of [[Accra]]. Sunny day flooding caused by sea level rise, increases [[coastal erosion]] that destroys housing, infrastructure and natural ecosystems. A number of communities in Coastal Ghana are already experiencing the changing tides.]]

In [[Africa]], future [[population growth]] amplifies risks from sea level rise. Some 54.2&nbsp;million people lived in the highly exposed low elevation coastal zones (LECZ) around 2000. This number will effectively double to around 110 million people by 2030, and then reach 185 to 230&nbsp;million people by 2060. By then, the average regional sea level rise will be around 21&nbsp;cm, with little difference from climate change scenarios.<ref name="AR6_WGII_Chapter9" /> By 2100, [[Egypt]], [[Mozambique]] and [[Tanzania]] are likely to have the largest number of people affected by annual flooding amongst all African countries. And under RCP8.5, 10 important cultural sites would be at risk of flooding and erosion by the end of the century.<ref name="AR6_WGII_Chapter9" />

In the near term, some of the largest displacement is projected to occur in the [[East Africa]] region. At least 750,000 people there are likely to be displaced from the coasts between 2020 and 2050. By 2050, 12 major African cities would collectively sustain cumulative damages of US$65&nbsp;billion for the "moderate" climate change scenario RCP4.5 and between US$86.5&nbsp;billion to US$137.5&nbsp;billion on average: in the worst case, these damages could effectively triple.<ref name="AR6_WGII_Chapter9" /> In all of these estimates, around half of the damages would occur in the Egyptian city of Alexandria.<ref name="AR6_WGII_Chapter9" /> Hundreds of thousands of people in its low-lying areas may already need relocation in the coming decade.<ref name="Michaelson-2018">{{cite news |url=https://www.theguardian.com/global-development/2018/aug/29/alexandria-little-venice-egypt-climate-change-frontline|title=Houses claimed by the canal: life on Egypt's climate change frontline| last=Michaelson| first=Ruth|date=25 August 2018|work=[[The Guardian]]|access-date=30 August 2018}}</ref> Across [[sub-Saharan Africa]] as a whole, damage from sea level rise could reach 2–4% of [[GDP]] by 2050, although this depends on the extent of future [[economic growth]] and [[climate change adaptation]].<ref name="AR6_WGII_Chapter9" />

=== Asia ===
{{Further|Climate change in Asia#Sea level rise}}

[[File:20091011松川浦.jpg|thumb|upright=1.3|Matsukawaura [[Lagoon]], located in [[Fukushima Prefecture]] of Honshu Island]]

[[File:Urban-Rural Population and Land Area Estimates, v2, 2010 Bangladesh (13873798283).jpg|thumb|upright=1.35|2010 estimates of population exposure to sea level rise in Bangladesh]]

Asia has the largest population at risk from sea level due to its dense coastal populations. As of 2022, some 63 million people in [[East Asia|East]] and [[South Asia]] were already at risk from a [[100-year flood]]. This is largely due to inadequate coastal protection in many countries. [[Bangladesh]], [[China]], [[India]], [[Indonesia]], [[Japan]], [[Pakistan]], the [[Philippines]], [[Thailand]] and [[Vietnam]] alone account for 70% of people exposed to sea level rise during the 21st century.<ref name="AR6_WGII_Chapter10" /><ref>{{Cite journal|last=McLeman|first=Robert|date=2018|title=Migration and displacement risks due to mean sea-level rise|journal=Bulletin of the Atomic Scientists|volume=74|issue=3|pages=148–154|doi=10.1080/00963402.2018.1461951|issn=0096-3402|bibcode=2018BuAtS..74c.148M|s2cid=150179939}}</ref> [[Climate change in Bangladesh|Sea level rise in Bangladesh]] is likely to displace 0.9-2.1&nbsp;million people by 2050. It may also force the relocation of up to one third of power plants as early as 2030, and many of the remaining plants would have to deal with the increased salinity of their cooling water.<ref name="AR6_WGII_Chapter10" /><ref name="DeLellis2021">{{cite journal |last1=De Lellis |first1=Pietro |last2=Marín |first2=Manuel Ruiz |last3=Porfiri |first3=Maurizio |date=29 March 2021 |title=Modeling Human Migration Under Environmental Change: A Case Study of the Effect of Sea Level Rise in Bangladesh |url=https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020EF001931 |journal=Earth's Future |volume=9 |issue=4 |pages=e2020EF001931 |doi=10.1029/2020EF001931 |bibcode=2021EaFut...901931D |hdl=10317/13078 |s2cid=233626963}}</ref> Nations like Bangladesh, Vietnam and China with extensive rice production on the coast are already seeing adverse impacts from saltwater intrusion.<ref>{{Cite web|url=http://www.fao.org/nr/climpag/pub/EIre0047_en.asp|title=Potential Impacts of Sea-Level Rise on Populations and Agriculture|website=www.fao.org|access-date=2018-10-21|archive-date=2020-04-18|archive-url=https://web.archive.org/web/20200418035608/http://www.fao.org/nr/climpag/pub/eire0047_en.asp}}</ref>

Modelling results predict that Asia will suffer direct economic damages of US$167.6&nbsp;billion at 0.47 meters of sea level rise. This rises to US$272.3&nbsp;billion at 1.12 meters and US$338.1&nbsp;billion at 1.75 meters. There is an additional indirect impact of US$8.5, 24 or 15&nbsp;billion from population displacement at those levels. China, India, the [[Republic of Korea]], Japan, Indonesia and [[Russia]] experience the largest economic losses.<ref name="AR6_WGII_Chapter10">Shaw, R., Y. Luo, T. S. Cheong, S. Abdul Halim, S. Chaturvedi, M. Hashizume, G. E. Insarov, Y. Ishikawa, M. Jafari, A. Kitoh, J. Pulhin, C. Singh, K. Vasant, and Z. Zhang, 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_Chapter10.pdf Chapter 10: Asia]. In [https://www.ipcc.ch/report/ar6/wg2/ Climate Change 2022: Impacts, Adaptation and Vulnerability] [H.-O. Pörtner, D. C. Roberts, M. Tignor, E. S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, New York, US, pp. 1457–1579 |doi=10.1017/9781009325844.012.</ref> Out of the 20 coastal cities expected to see the highest flood losses by 2050, 13 are in Asia. Nine of these are the so-called [[sinking cities]], where [[subsidence]] (typically caused by unsustainable [[groundwater]] extraction in the past) would compound sea level rise. These are [[Bangkok]], [[Guangzhou]], [[Ho Chi Minh City]], [[Jakarta]], [[Kolkata]], [[Nagoya]], [[Tianjin]], [[Xiamen]] and [[Zhanjiang]].<ref>{{Cite journal|last1=Erkens|first1=G.|last2=Bucx|first2=T.|last3=Dam|first3=R.|last4=de Lange|first4=G.|last5=Lambert|first5=J.|date=2015-11-12|title=Sinking coastal cities|url=https://piahs.copernicus.org/articles/372/189/2015/|journal=Proceedings of the International Association of Hydrological Sciences|language=en|volume=372|pages=189–198|doi=10.5194/piahs-372-189-2015|bibcode=2015PIAHS.372..189E|issn=2199-899X |doi-access=free}}</ref>

By 2050, Guangzhou would see 0.2 meters of sea level rise and estimated ''annual'' economic losses of US$254 million – the highest in the world.<ref name="AR6_WGII_Chapter10" /> In [[Shanghai]], coastal inundation amounts to about 0.03% of local [[GDP]], yet would increase to 0.8% by 2100 even under the "moderate" [[Representative Concentration Pathway|RCP4.5]] scenario in the absence of adaptation.<ref name="AR6_WGII_Chapter10" /> The city of [[Jakarta]] is [[Flooding in Jakarta|sinking]] so much (up to {{cvt|28|cm|in|frac=2}} per year between 1982 and 2010 in some areas<ref>{{cite journal |last1=Abidin |first1=Hasanuddin Z. |last2=Andreas |first2=Heri |last3=Gumilar |first3=Irwan |last4=Fukuda |first4=Yoichi |last5=Pohan |first5=Yusuf E. |last6=Deguchi |first6=T. |title=Land subsidence of Jakarta (Indonesia) and its relation with urban development |journal=Natural Hazards |date=11 June 2011 |volume=59 |issue=3 |pages=1753–1771 |doi=10.1007/s11069-011-9866-9 |bibcode=2011NatHa..59.1753A |s2cid=129557182}}</ref>) that in 2019, the government had committed to relocate the [[capital of Indonesia]] to another city.<ref>{{Cite news|url=https://www.washingtonpost.com/opinions/2019/05/03/seas-rise-indonesia-is-moving-its-capital-city-other-cities-should-take-note/|title=As seas rise, Indonesia is moving its capital city. Other cities should take note.|last=Englander|first=John|date=3 May 2019|newspaper=[[The Washington Post]]|access-date=31 August 2019}}</ref>

=== Australasia ===
[[File:King's Beach since Friday 14th April, 2006 - panoramio.jpg|thumb|left|King's Beach at [[Caloundra]]]]

In [[Australia]], erosion and flooding of [[Queensland]]'s [[Sunshine Coast, Queensland|Sunshine Coast]] beaches is likely to intensify by 60% by 2030. Without adaptation there would be a big impact on tourism. Adaptation costs for sea level rise would be three times higher under the high-emission [[Representative Concentration Pathway|RCP]]8.5 scenario than in the low-emission RCP2.6 scenario. Sea level rise of 0.2-0.3 meters is likely by 2050. In these conditions what is currently a [[100-year flood]] would occur every year in the [[New Zealand]] cities of [[Wellington]] and [[Christchurch]]. With 0.5 m sea level rise, a current 100-year flood in Australia would occur several times a year. In New Zealand this would expose buildings with a collective worth of NZ$12.75&nbsp;billion to new 100-year floods. A meter or so of sea level rise would threaten assets in New Zealand with a worth of NZD$25.5&nbsp;billion. There would be a disproportionate impact on [[Māori people|Maori]]-owned holdings and cultural heritage objects. Australian assets worth AUS$164–226&nbsp;billion including many [[unsealed road]]s and [[railway line]]s would also be at risk. This amounts to a 111% rise in Australia's inundation costs between 2020 and 2100.<ref name="AR6_WGII_Chapter11">Lawrence, J., B. Mackey, F. Chiew, M.J. Costello, K. Hennessy, N. Lansbury, U.B. Nidumolu, G. Pecl, L. Rickards, N. Tapper,
A. Woodward, and A. Wreford, 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_Chapter11.pdf Chapter 11: Australasia]. In [https://www.ipcc.ch/report/ar6/wg2/ Climate Change 2022: Impacts, Adaptation and Vulnerability] [H.-O. Pörtner, D.C. Roberts, M. Tignor, E.S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, US, pp. 1581–1688,
|doi=10.1017/9781009325844.013</ref>

=== Central and South America ===
[[File:Santos Aérea (cropped).jpg|thumb|An aerial view of [[São Paulo]]'s Port of Santos]]

By 2100, coastal flooding and erosion will affect at least 3-4&nbsp;million people in [[South America]]. Many people live in low-lying areas exposed to sea level rise. This includes 6% of the population of [[Venezuela]], 56% of the population of [[Guyana]] and 68% of the population of [[Suriname]]. In Guyana much of the capital [[Georgetown, Guyana|Georgetown]] is already below sea level. In [[Brazil]], the coastal ecoregion of [[Caatinga]] is responsible for 99% of its [[shrimp]] production. A combination of sea level rise, ocean warming and [[ocean acidification]] threaten its unique. Extreme wave or wind behavior disrupted the port complex of [[Santa Catarina (island)|Santa Catarina]] 76 times in one 6-year period in the 2010s. There was a US$25,000-50,000 loss for each idle day. In [[Port of Santos]], [[storm surge]]s were three times more frequent between 2000 and 2016 than between 1928 and 1999.<ref name="AR6_WGII_Chapter12">Castellanos, E., M.F. Lemos, L. Astigarraga, N. Chacón, N. Cuvi, C. Huggel, L. Miranda, M. Moncassim Vale, J.P. Ometto,
P.L. Peri, J.C. Postigo, L. Ramajo, L. Roco, and M. Rusticucci, 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_Chapter12.pdf Chapter 12: Central and South America]. In [https://www.ipcc.ch/report/ar6/wg2/ Climate Change 2022: Impacts, Adaptation and Vulnerability] [H.-O. Pörtner, D.C. Roberts, M. Tignor, E.S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, US, pp. 1689–1816 |doi=10.1017/9781009325844.014</ref>

=== Europe ===
[[File:Beach restoration device.jpg|thumb|left|[[Beach nourishment]] in progress in [[Barcelona]].]]

Many sandy coastlines in [[Europe]] are vulnerable to erosion due to sea level rise. In [[Spain]], [[Costa del Maresme]] is likely to retreat by 16 meters by 2050 relative to 2010. This could amount to 52 meters by 2100 under RCP8.5<ref>{{cite journal |last1=Ballesteros |first1=Caridad |last2=Jiménez |first2=José A. |last3=Valdemoro |first3=Herminia I. |last4=Bosom |first4=Eva |date=7 September 2017 |title=Erosion consequences on beach functions along the Maresme coast (NW Mediterranean, Spain) |url=https://link.springer.com/article/10.1007/s11069-017-3038-5 |journal=Natural Hazards |language=en |volume=90 |pages=173–195 |doi=10.1007/s11069-017-3038-5 |s2cid=135328414}}</ref> Other vulnerable coastlines include the [[Tyrrhenian Sea]] coast of [[Italy]]'s [[Calabria]] region,<ref>{{cite journal |last1=Ietto |first1=Fabio |last2=Cantasano |first2=Nicola |last3=Pellicone |first3=Gaetano |date=11 April 2018 |title=A New Coastal Erosion Risk Assessment Indicator: Application to the Calabria Tyrrhenian Littoral (Southern Italy) |url=https://link.springer.com/article/10.1007/s40710-018-0295-6 |journal=Environmental Processes |language=en |volume=5 |issue=2 |pages=201–223 |doi=10.1007/s40710-018-0295-6 |bibcode=2018EProc...5..201I |s2cid=134889581}}</ref> the Barra-Vagueira coast in [[Portugal]]<ref>{{cite journal |last1=Ferreira |first1=A. M. |last2=Coelho |first2=C. |last3=Narra |first3=P. |date=13 October 2020 |title=Coastal erosion risk assessment to discuss mitigation strategies: Barra-Vagueira, Portugal |url=https://link.springer.com/article/10.1007/s11069-020-04349-2 |journal=Natural Hazards |language=en |volume=105 |pages=1069–1107 |doi=10.1007/s11069-020-04349-2 |s2cid=222318289}}</ref> and Nørlev Strand in [[Denmark]].<ref>{{cite journal |last1=Rivero |first1=Ofelia Yocasta |last2=Margheritini |first2=Lucia |last3=Frigaard |first3=Peter |date=4 February 2021 |title=Accumulated effects of chronic, acute and man-induced erosion in Nørlev strand on the Danish west coast |url=https://link.springer.com/article/10.1007/s11852-021-00812-9 |journal=Journal of Coastal Conservation |language=en |volume=25 |issue=1 |page=24 |doi=10.1007/s11852-021-00812-9 |bibcode=2021JCC....25...24R |s2cid=231794192}}</ref>

In France, it was estimated that 8,000-10,000 people would be forced to migrate away from the coasts by 2080.<ref>{{Cite journal|last1=Tierolf|first1=Lars|last2=Haer|first2=Toon Haer|last3=Wouter Botzen|first3=W. J.|last4=de Bruijn|first4=Jens A. |last5=Ton |first5=Marijn J. |last6=Reimann|first6=Lena|last7=Aerts |first7=Jeroen C. J. H. |date=13 March 2023|title=A coupled agent-based model for France for simulating adaptation and migration decisions under future coastal flood risk|journal=Scientific Reports|volume=13 |issue=1 |page=4176 |doi=10.1038/s41598-023-31351-y |pmid=36914726 |pmc=10011601 |bibcode=2023NatSR..13.4176T}}</ref> The Italian city of [[Venice]] is located on islands. It is highly [[Flooding in Venice|vulnerable to flooding]] and has already spent $6&nbsp;billion on a barrier system.<ref>{{cite news |last1=Calma |first1=Justine |title=Venice's historic flooding blamed on human failure and climate change |url=https://www.theverge.com/2019/11/14/20963878/venice-high-tide-climate-change-flood-barrier-sea-levels |access-date=17 November 2019 |agency=The Verge |date=November 14, 2019}}</ref><ref>{{cite news |last1=Shepherd |first1=Marshall |title=Venice Flooding Reveals A Real Hoax About Climate Change - Framing It As "Either/Or" |url=https://www.forbes.com/sites/marshallshepherd/2019/11/16/venice-flooding-reveals-a-real-hoax-about-climate-changeframing-it-as-eitheror/ |access-date=17 November 2019 |agency=Forbes |date=16 November 2019}}</ref> A quarter of the German state of [[Schleswig-Holstein]], inhabited by over 350,000 people, is at low elevation and has been vulnerable to flooding since preindustrial times. Many [[levee]]s already exist. Because of its complex geography, the authorities chose a flexible mix of hard and soft measures to cope with sea level rise of over 1 meter per century.<ref name="Hurk2022">{{Cite journal|last1=van der Hurk|first1=Bart|last2=Bisaro|first2=Alexander|last3=Haasnoot|first3=Marjolijn|last4=Nicholls|first4=Robert J. |last5=Rehdanz |first5=Katrin |last6=Stuparu|first6=Dana|date=28 January 2022|title=Living with sea-level rise in North-West Europe: Science-policy challenges across scales|journal=Climate Risk Management|volume=35|page=100403 |doi=10.1016/j.crm.2022.100403 |bibcode=2022CliRM..3500403V |s2cid=246354121}}</ref> In the [[United Kingdom]], sea level at the end of the century would increase by 53 to 115 centimeters at the mouth of the River [[Thames]] and 30 to 90 centimeters at [[Edinburgh]].<ref>{{cite journal |last1=Howard |first1=Tom |last2=Palmer |first2=Matthew D |last3=Bricheno |first3=Lucy M |date=18 September 2019 |title=Contributions to 21st century projections of extreme sea-level change around the UK |url=https://iopscience.iop.org/article/10.1088/2515-7620/ab42d7 |journal=Environmental Research Communications |language=en |volume=1 |issue=9 |page=095002 |doi=10.1088/2515-7620/ab42d7 |bibcode=2019ERCom...1i5002H |s2cid=203120550}}</ref> The UK has divided its coast into 22 areas, each covered by a Shoreline Management Plan. Those are sub-divided into 2000 management units, working across three periods of 0–20, 20-50 and 50–100 years.<ref name="Hurk2022" />

The [[Netherlands]] is a country that sits partially below sea level and is subsiding. It has responded by extending its [[Delta Works]] program.<ref>{{Cite news|url=https://www.nytimes.com/interactive/2017/06/15/world/europe/climate-change-rotterdam.html,%20https://www.nytimes.com/interactive/2017/06/15/world/europe/climate-change-rotterdam.html|title=The Dutch Have Solutions to Rising Seas. The World Is Watching.|last1=Kimmelman|first1=Michael|date=2017-06-15|work=The New York Times|access-date=2019-02-02|last2=Haner|first2=Josh|issn=0362-4331}}</ref> Drafted in 2008, the ''Delta Commission'' report said that the country must plan for a rise in the [[North Sea]] up to {{convert|1.3|m|ftin|abbr=on}} by 2100 and plan for a {{convert|2 - 4|m|ft|0|sigfig=1|abbr=on}} rise by 2200.<ref>{{Cite news|url=https://www.nytimes.com/2008/09/03/news/03iht-03dutch.15877468.html|title=Dutch draw up drastic measures to defend coast against rising seas|date=3 September 2008|work=[[The New York Times]]}}</ref> It advised annual spending between €1.0 and €1.5&nbsp;billion. This would support measures such as broadening coastal [[dunes]] and strengthening sea and river [[Dyke (construction)|dikes]]. Worst-case evacuation plans were also drawn up.<ref>{{cite news |title=Rising Sea Levels Threaten Netherlands |url=https://www.newspapers.com/image/514725270/ |access-date=28 October 2022 |work=National Post |agency=Agence France-Presse |date=September 4, 2008 |location=Toronto |page=AL12}}</ref>

=== North America ===
[[File:October 17 2016 sunny day tidal flooding at Brickell Bay Drive and 12 Street downtown Miami, 4.34 MLLW high tide am.jpg|thumb|[[Tidal flooding]] in [[Climate of Miami|Miami]] during a [[king tide]] (October 17, 2016). The risk of tidal flooding increases with sea level rise.]]

As of 2017, around 95 million Americans lived on the coast. The figures for [[Canada]] and [[Mexico]] were 6.5 million and 19 million. Increased chronic [[nuisance flooding]] and [[king tide]] flooding is already a problem in the highly [[Climate change vulnerability|vulnerable]] state of [[Florida]].<ref>{{Cite web|date=2020-02-10|title=Florida Coastal Flooding Maps: Residents Deny Predicted Risks to Their Property|url=https://www.ecowatch.com/florida-coastal-flooding-maps-2645087745.html|access-date=2021-01-31|website=EcoWatch|language=en}}</ref> The [[US East Coast]] is also vulnerable.<ref>{{cite journal|last1=Sweet & Park |title=Increased nuisance flooding along the coasts of the United States due to sea level rise: Past and future |journal=Geophysical Research Letters |year=2015 |volume=42 |issue=22 |pages=9846–9852 |doi=10.1002/2015GL066072 |bibcode=2015GeoRL..42.9846M |s2cid=19624347}}</ref> On average, the number of days with [[tidal flooding]] in the US increased 2 times in the years 2000–2020, reaching 3–7 days per year. In some areas the increase was much stronger: 4 times in the Southeast Atlantic and 11 times in the Western Gulf. By the year 2030 the average number is expected to be 7–15 days, reaching 25–75 days by 2050.<ref>{{cite web |title=High Tide Flooding |url=https://coast.noaa.gov/states/fast-facts/recurrent-tidal-flooding.html |website=NOAA |access-date=10 July 2023}}</ref> U.S. coastal cities have responded with [[beach nourishment]] or ''beach replenishment.'' This trucks in mined sand in addition to other adaptation measures such as zoning, restrictions on state funding, and building code standards.<ref name="ClimateCentral2012">{{cite web|url=http://www.climatecentral.org/news/its-beach-season-enjoy-it-while-you-can|title=Climate Change, Sea Level Rise Spurring Beach Erosion|year=2012|website=Climate Central}}</ref><ref>{{Cite journal|last=Carpenter|first=Adam T.|date=2020-05-04|title=Public priorities on locally-driven sea level rise planning on the East Coast of the United States|journal=PeerJ|language=en|volume=8|pages=e9044|doi=10.7717/peerj.9044|pmid=32411525|pmc=7204830|issn=2167-8359 |doi-access=free}}</ref>

Along an estimated ~15% of the US coastline, the majority of local [[groundwater]] levels are already below sea level. This places those groundwater reservoirs at risk of sea water intrusion. That would render fresh water unusable once its concentration exceeds 2-3%.<ref>{{cite journal |last1=Jasechko |first1=Scott J.|last2=Perrone |first2=Debra |last3=Seybold |first3=Hansjörg |last4=Fan |first4=Ying |last5=Kirchner |first5=James W. |title=Groundwater level observations in 250,000 coastal US wells reveal scope of potential seawater intrusion |date=26 June 2020 |journal=Nature Communications |volume=11 |issue=1 |page=3229 |doi=10.1038/s41467-020-17038-2 |pmid=32591535 |pmc=7319989 |bibcode=2020NatCo..11.3229J}}</ref> Damage is also widespread in Canada. It will affect major cities like [[Halifax, Nova Scotia|Halifax]] and more remote locations like [[Lennox Island (Prince Edward Island)|Lennox Island]]. The [[Mi'kmaq]] [[Lennox Island First Nation|community]] there is already considering relocation due to widespread coastal erosion. In Mexico, damage from SLR to [[tourism]] hotspots like [[Cancun]], [[Isla Mujeres]], [[Playa del Carmen]], [[Puerto Morelos]] and [[Cozumel]] could amount to US$1.4–2.3&nbsp;billion.<ref name="AR6_WGII_Chapter14" /> The increase in [[storm surge]] due to sea level rise is also a problem. Due to this effect [[Hurricane Sandy]] caused an additional US$8 billion in damage, impacted 36,000 more houses and 71,000 more people.<ref>{{cite journal |title=Economic damages from Hurricane Sandy attributable to sea level rise caused by anthropogenic climate change |journal=Nature Communications |date=18 May 2021 |volume=12 |bibcode=2021NatCo..12.2720S |last1=Strauss |first1=Benjamin H. |last2=Orton |first2=Philip M. |last3=Bittermann |first3=Klaus |last4=Buchanan |first4=Maya K. |last5=Gilford |first5=Daniel M. |last6=Kopp |first6=Robert E. |last7=Kulp |first7=Scott |last8=Massey |first8=Chris |last9=Moel |first9=Hans de |last10=Vinogradov |first10=Sergey |issue=1 |page=2720 |doi=10.1038/s41467-021-22838-1 |pmid=34006886 |pmc=8131618 |s2cid=234783225}}</ref><ref>{{cite news |last1=Seabrook |first1=Victoria |title=Climate change to blame for $8 billion of Hurricane Sandy losses, study finds |url=https://news.sky.com/story/climate-change-to-blame-for-8-billion-of-hurricane-sandy-losses-study-finds-12309974#:~:text=The%20raised%20water%20levels%20allowed,36%2C000%20homes%20and%2071%2C000%20people. |access-date=9 July 2023 |agency=Sky News |publisher=Nature Communications |date=19 May 2021}}</ref> In the future, the northern [[Gulf of Mexico]], [[Atlantic Canada]] and the [[Pacific coast of Mexico]] would experience the greatest sea level rise. By 2030, flooding along the US [[Gulf Coast]] could cause economic losses of up to US$176&nbsp;billion. Using [[nature-based solutions]] like [[wetland restoration]] and [[oyster reef]] restoration could avoid around US$50 billion of this.<ref name="AR6_WGII_Chapter14" />

[[File:2050 Projected sea level rise - United States coasts - NOAA.svg|thumb|upright=1.35|left|[[NOAA]] predicts different levels of sea level rise through 2050 for several US coastlines.<ref name=NOAA-2022 />|alt=A comparison of SLR in six parts of the US. The Gulf Coast and East Coast see the most SLR, whereas the West Coast the least]]

By 2050, coastal flooding in the US is likely to rise tenfold to four "moderate" flooding events per year. That forecast is even without storms or heavy rainfall.<ref>{{cite web |title=U.S Coastline to See Up to a Foot of Sea Level by 2050 |url=https://www.noaa.gov/news-release/us-coastline-to-see-up-to-foot-of-sea-level-rise-by-2050 |access-date=February 16, 2022 |website=National Oceanic and Atmospheric Administration|date=15 February 2022}}</ref><ref>{{cite web |date=2022 |title=More Damaging Flooding, 2022 Sea Level Rise Technical Report |url=https://oceanservice.noaa.gov/hazards/sealevelrise/sealevelrise-tech-report.html#step2 |access-date=2022-03-18 |website=National Ocean Service, [[NOAA]]}}</ref> In [[New York City]], current [[100-year flood]] would occur once in 19–68 years by 2050 and 4–60 years by 2080.<ref>{{cite web|last=Gornitz|first=Vivien|date=2002|title=Impact of Sea Level Rise in the New York City Metropolitan Area|url=https://eportfolios.macaulay.cuny.edu/bird2012/files/2012/07/Impacts-of-SLR-in-the-NYC-Metropolitan-Area.-pdf.pdf|access-date=2020-08-09|website=Global and Planetary Change|archive-date=2019-09-26|archive-url=https://web.archive.org/web/20190926115312/https://eportfolios.macaulay.cuny.edu/bird2012/files/2012/07/Impacts-of-SLR-in-the-NYC-Metropolitan-Area.-pdf.pdf|url-status=dead}}</ref> By 2050, 20&nbsp;million people in the greater [[New York City]] area would be at risk. This is because 40% of existing [[water treatment]] facilities would be compromised and 60% of [[power plant]]s will need relocation.

By 2100, sea level rise of {{cvt|0.9|m|ft|frac=2}} and {{cvt|1.8|m|ft|frac=2}} would threaten 4.2 and 13.1&nbsp;million people in the US, respectively. In [[California]] alone, {{cvt|2|m|ft|frac=2}} of SLR could affect 600,000 people and threaten over US$150&nbsp;billion in property with inundation. This potentially represents over 6% of the state's [[GDP]]. In [[North Carolina]], a meter of SLR inundates 42% of the [[Albemarle-Pamlico Peninsula]], costing up to US$14&nbsp;billion. In nine southeast US states, the same level of sea level rise would claim up to 13,000 historical and archaeological sites, including over 1000 sites eligible for inclusion in the [[National Register for Historic Places]].<ref name="AR6_WGII_Chapter14">Hicke, J.A., S. Lucatello, L.D., Mortsch, J. Dawson, M. Domínguez Aguilar, C.A.F. Enquist, E.A. Gilmore, D.S. Gutzler, S. Harper, K. Holsman, E.B. Jewett, T.A. Kohler, and KA. Miller, 2022: [https://www.ipcc.ch/report/ar6/wg2/downloads/report/IPCC_AR6_WGII_Chapter14.pdf Chapter 14: North America]. In [https://www.ipcc.ch/report/ar6/wg2/ Climate Change 2022: Impacts, Adaptation and Vulnerability] [H.-O. Pörtner, D.C. Roberts, M. Tignor, E.S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, US, pp. 1929–2042</ref>

=== Island nations ===
[[File:Malé.jpg|thumb|left|upright=1.4|[[Malé]], the capital island of [[Maldives]].]]

{{Further|Effects of climate change on island nations|Small Island Developing States|Alliance of Small Island States}}

Small island states are nations with populations on [[atoll]]s and other [[low island]]s. Atolls on average reach {{convert|3-6|ft|m|1|order=flip|abbr=on}} above sea level.<ref>{{Cite web|title=Many Low-Lying Atoll Islands Will Be Uninhabitable by Mid-21st Century {{!}} U.S. Geological Survey|url=https://www.usgs.gov/news/national-news-release/many-low-lying-atoll-islands-will-be-uninhabitable-mid-21st-century|access-date=2021-12-17|website=www.usgs.gov}}</ref> These are the most vulnerable places to [[coastal erosion]], flooding and salt intrusion [[Soil salinization|into soils]] and freshwater caused by sea level rise. Sea level rise may make an island uninhabitable before it is completely flooded.<ref>{{Cite journal|last1=Zhu|first1=Bozhong|last2=Bai|first2=Yan|last3=He|first3=Xianqiang|last4=Chen|first4=Xiaoyan|last5=Li|first5=Teng|last6=Gong|first6=Fang|date=2021-09-18|title=Long-Term Changes in the Land–Ocean Ecological Environment in Small Island Countries in the South Pacific: A Fiji Vision|journal=Remote Sensing|language=en|volume=13|issue=18|page=3740|doi=10.3390/rs13183740|bibcode=2021RemS...13.3740Z|issn=2072-4292|doi-access=free}}</ref> Already, children in small island states encounter hampered access to food and water. They suffer an increased rate of mental and social disorders due to these stresses.<ref>{{Cite journal|last1=Sly|first1=Peter D|last2=Vilcins|first2=Dwan|date=November 2021|title=Climate impacts on air quality and child health and wellbeing: Implications for Oceania|url=https://onlinelibrary.wiley.com/doi/10.1111/jpc.15650|journal=Journal of Paediatrics and Child Health|language=en|volume=57|issue=11|pages=1805–1810|doi=10.1111/jpc.15650|pmid=34792251|s2cid=244271480|issn=1034-4810}}</ref> At current rates, sea level rise would be high enough to make the Maldives uninhabitable by 2100.<ref>{{cite web |author=Megan Angelo |date=1 May 2009 |title=Honey, I Sunk the Maldives: Environmental changes could wipe out some of the world's most well-known travel destinations |url=http://travel.yahoo.com/p-interests-27384279;_ylc=X3oDMTFxcWIyczFpBF9TAzI3MTYxNDkEX3MDMjcxOTQ4MQRzZWMDZnAtdG9kYXltb2QEc2xrA21hbGRpdmVzLTQtMjgtMDk- |archive-url=https://web.archive.org/web/20120717041919/http://travel.yahoo.com/p-interests-27384279 |archive-date=17 July 2012 |access-date=29 September 2009}}</ref><ref>{{cite web |author=Kristina Stefanova |date=19 April 2009 |title=Climate refugees in Pacific flee rising sea |url=http://www.washingtontimes.com/news/2009/apr/19/rising-sea-levels-in-pacific-create-wave-of-migran/ |website=[[The Washington Times]]}}</ref> Five of the [[Solomon Islands]] have already disappeared due to the effects of sea level rise and stronger trade winds pushing water into the [[Western Pacific Ocean|Western Pacific]].<ref>{{Cite web |last=Klein |first=Alice |title=Five Pacific islands vanish from sight as sea levels rise |url=https://www.newscientist.com/article/2087356-five-pacific-islands-vanish-from-sight-as-sea-levels-rise/ |access-date=2016-05-09 |website=New Scientist}}</ref>
[[File:Island area change in the Central Pacific and Solomon Islands - erlaa21eff7 hr.jpg|thumb|upright=1.6|Surface area change of islands in the [[List of islands in the Pacific Ocean|Central Pacific]] and [[Solomon Islands]]<ref name="Albeert2016">{{Cite Q|Q29028186}}</ref>]]

Adaptation to sea level rise is costly for small island nations as a large portion of their population lives in areas that are at risk.<ref>{{Cite book|chapter-url=http://www.ipcc.ch/pdf/assessment-report/ar5/wg2/WGIIAR5-Chap29_FINAL.pdf|title=AR5 WGII|last1=Nurse|first1=Leonard A.|last2=McLean|first2=Roger|publisher=Cambridge University Press|year=2014|editor-last=Barros|editor-first=VR|chapter=29: Small Islands|editor-last2=Field|access-date=2018-09-02|archive-date=2018-04-30|archive-url=https://web.archive.org/web/20180430194832/http://www.ipcc.ch/pdf/assessment-report/ar5/wg2/WGIIAR5-Chap29_FINAL.pdf}}</ref> Nations like [[Maldives]], [[Kiribati]] and [[Tuvalu]] already have to consider controlled international migration of their population in response to rising seas.<ref name="Grecequet2017" /> The alternative of uncontrolled migration threatens to worsen the humanitarian crisis of [[Climate migrant|climate refugees]].<ref>{{Cite web|last=Nations|first=United|title=Small Islands, Rising Seas|url=https://www.un.org/en/chronicle/article/small-islands-rising-seas|access-date=2021-12-17|website=United Nations|language=en}}</ref> In 2014, Kiribati purchased 20 square kilometers of land (about 2.5% of Kiribati's current area) on the [[Fiji]]an island of [[Vanua Levu]] to relocate its population once their own islands are lost to the sea.<ref>{{cite news|url=https://www.theguardian.com/environment/2014/jul/01/kiribati-climate-change-fiji-vanua-levu|title=Besieged by the rising tides of climate change, Kiribati buys land in Fiji|last1=Caramel|first1=Laurence|date=July 1, 2014|access-date=9 January 2023|agency=The Guardian}}</ref>

[[Fiji]] also suffers from sea level rise.<ref>{{Cite journal |last=Long |first=Maebh |author-link=Maebh Long |year=2018 |title=Vanua in the Anthropocene: Relationality and Sea Level Rise in Fiji |url=https://muse.jhu.edu/article/710005 |journal=Symplokē |volume=26 |issue=1–2 |pages=51–70 |doi=10.5250/symploke.26.1-2.0051 |s2cid=150286287}}</ref> It is in a comparatively safer position. Its residents continue to rely on local adaptation like moving further inland and increasing [[sediment]] supply to combat erosion instead of relocating entirely.<ref name="Grecequet2017">{{Cite web|url=http://theconversation.com/many-small-island-nations-can-adapt-to-climate-change-with-global-support-86820|title=Many small island nations can adapt to climate change with global support|last1=Grecequet|first1=Martina|last2=Noble|first2=Ian|date=2017-11-16|website=The Conversation|access-date=2019-02-02|last3=Hellmann|first3=Jessica}}</ref> Fiji has also issued a green bond of $50&nbsp;million to invest in green initiatives and fund adaptation efforts. It is restoring [[coral reef]]s and [[mangrove]]s to protect against flooding and erosion. It sees this as a more cost-efficient alternative to building [[sea wall]]s. The nations of [[Palau]] and [[Tonga]] are taking similar steps.<ref name="Grecequet2017" /><ref>{{Cite web|url=http://www.unenvironment.org/news-and-stories/video/adaptation-sea-level-rise|title=Adaptation to Sea Level Rise|date=2018-01-11|website=UN Environment|access-date=2019-02-02}}</ref> Even when an island is not threatened with complete disappearance from flooding, tourism and local economies may end up devastated. For instance, sea level rise of {{cvt|1.0|m|ftin|0}} would cause partial or complete inundation of 29% of coastal resorts in the [[Caribbean]]. A further 49&ndash;60% of coastal resorts would be at risk from resulting coastal erosion.<ref>{{Cite journal|last1=Thomas|first1=Adelle|last2=Baptiste|first2=April|last3=Martyr-Koller|first3=Rosanne|last4=Pringle|first4=Patrick|last5=Rhiney|first5=Kevon|date=2020-10-17|title=Climate Change and Small Island Developing States|journal=Annual Review of Environment and Resources|language=en|volume=45|issue=1|pages=1–27|doi=10.1146/annurev-environ-012320-083355|issn=1543-5938|doi-access=free}}</ref>

== See also ==
{{Portal|Oceans|Climate change|Energy|Renewable energy|Environment}}
* [[Climate emergency declaration]]
* [[Coastal development hazards]]
* [[Effects of climate change on oceans]]
* [[List of countries by average elevation]]
* [[Paleoclimate]]
* [[Rising Seas (song)]]

== References ==
{{Reflist}}

== External links ==
{{Wikibooks|Historical Geology|Sea level variations}}
* [https://climate.nasa.gov/vital-signs/sea-level/ Vital signs / Sea level]
* [https://sealevel.nasa.gov/ Sea level change / Observations from space] (links to multiple measurements)
* [https://science2017.globalchange.gov/chapter/12/ Fourth National Climate Assessment Sea Level Rise Key Message]
* [https://www.ngs.noaa.gov/PUBS_LIB/SLCScenariosLL.pdf Incorporating Sea Level Change Scenarios at the Local Level] Outlines eight steps a community can take to develop site-appropriate scenarios
* [https://gloss-sealevel.org/ The Global Sea Level Observing System (GLOSS)]
* [https://coast.noaa.gov/slr/ USA Sea Level Rise Viewer (NOAA)]

{{World topic|Sea level rise in|title=Sea level rise by country|noredlinks=yes|state=collapsed}}

[[Category:Articles containing video clips]]
[[Category:Climate change adaptation]]
[[Category:Coastal geography]]
[[Category:Effects of climate change]]
[[Category:Oceanography]]
[[Category:Sea level|Rise]]

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Interactions between sea-level rise and wave exposure on reef island dynamics in the Solomon Islands: Some statements, Title, Sitelink, Miscellaneous (e.g. aliases, entity existence)
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