Contents

Lamont–Doherty Earth Observatory

Lamont-Doherty Earth Observatory

Company type	Non-profit research institute
Founded	1948
Headquarters	Palisades, New York
Key people	Steven L. Goldstein, Interim Director [1]
Parent	Columbia University
Website	www.ldeo.columbia.edu

The Lamont-Doherty Earth Observatory (LDEO) is a research institution specializing in the Earth science and climate change. Though part of Columbia University, it is located on a separate closed campus in Palisades, New York.^[2]

The Observatory was one of the centers of research that led to the development of the theory of Plate Tectonics as well as many other notable scientific developments.

LDEO is located in Palisades, New York on a property overlooking the Hudson River which was once the weekend residence of banker Thomas W. Lamont. It was donated to the university in 1948 by his widow, Florence Lamont.^[2] In 1969, the Observatory was renamed "Lamont-Doherty" following a gift from the Henry L. and Grace Doherty Charitable Foundation.^[3]

The LDEO is a substantial source of data for the US government in relation to climate change. Faculty at the LDEO have been noted for giving climate change testimony to Congress in relation to melting ice sheets.^[4] NOAA has also noted the LDEO's Global Ocean Surface Water Partial Pressure of CO2 Database as being an instrumental source of partial pressure carbon dioxide data (pCO₂), which can, in turn, detail the amount of carbon dioxide dissolved in the earth's oceans. Many versions of the LDEO database have been published over the years, dating back to 2006.^[5]

The tree-ring lab at the LDEO studies the effects on climate and climate change on trees. In an interview, Nicole Davi from the LDEO noted findings like the formation of tree-rings during extended dry seasons, as well as work being done to carbon-date trees to verify tree ring data.^[6]

The core repository at the LDEO stores various drilled sediment samples from the earth's oceans. The samples have been used to detail climate changes between glaciation periods, in context of dissolved elements and gases, like calcium (from shells) and carbon dioxide.^[7]

A major source of past earthquake data comes from the Lamont-Doherty Earth Observatory/National Center for Earthquake Engineering Research (NCEER) Earthquake Strong Motion Database.^[8]

In 2012, Voice of America documented the work done by LDEO researcher Robin Bell, and others, in mapping the land underneath the Antarctica ice sheet. Several notable findings included the discovery of hidden rivers, hidden mountain ranges, and significant geothermal energy below the ice.^[9]

Some notable papers from the LDEO include analysis of:

• Seismic activity following nuclear weapons testing.^[13][14]
• Continental drift: in the North Atlantic,^[15] and, separately, their effects on the magnetic field.^{[16][verification needed]}
• The "ocean-atmosphere system."^[17]
• Future weather in El Niño events.^[18]
• The relationship between weather and yields.^[19]
• The relationship between rotation of the core and seismic activity.^[20][21]
• The sea floor.^[22]
• Ice ages.^{[23][24][verification needed][25]}
• Solar weather.^[26]
• Seismic activity on the moon.^[27]

• Maurice Ewing - first director of the Observatory (1949 - 1972)
• Wallace Smith Broecker - popularized the term Global warming
• Marie Tharp - oceanic cartographer whose work led to the consensus on the plate tectonics and continental drift theories.^[28][29]
• Bruce C. Heezen
• Maureen Raymo - director of the Observatory
• Robin Bell
• Sean Solomon - directory of the Observatory
• Terry Plank

Wikimedia Commons has media related to Lamont–Doherty Earth Observatory.

• Lamont-Doherty Earth Observatory Website

41°00′14″N 73°54′25″W / 41.004°N 73.907°W / 41.004; -73.907