Steppe in Mongolia
 |
This article needs additional citations for verification. Please help improve this articlebyadding citations to reliable sources. Unsourced material may be challenged and removed.
Find sources: "Steppe" – news · newspapers · books · scholar · JSTOR (February 2014) (Learn how and when to remove this message) |
Inphysical geography, a steppe (/stɛp/) is an ecoregion characterized by grassland plains without closed forests except near rivers and lakes.[1] Steppe biomes may include:
A steppe is usually covered with grass and shrubs, depending on the season and latitude. The term steppe climate denotes a semi-arid climate, which is encountered in regions too dry to support a forest, but not dry enough to be a desert.
Steppes are usually characterized by a semi-arid or continental[citation needed] climate. Extremes can be recorded in the summer of up to 45 °C (115 °F) and in winter of down to −55 °C (−65 °F). Besides this major seasonal difference, fluctuations between day and night are also significant. In both the highlands of Mongolia and northern Nevada, 30 °C (85 °F) can be reached during the day with sub-freezing readings at night.
Steppes average 250–500 mm (10–20 in) of annual precipitation and feature hot summers and cold winters when located in mid-latitudes. In addition to the precipitation level, its combination with potential evapotranspiration defines a steppe climate.
Steppe can be classified by climate:[2]
It can also be classified by vegetation type, e.g. shrub-steppe and alpine-steppe.
The world's largest steppe region, often referred to as "the Great Steppe", is found in Eastern Europe and Central Asia, and neighbouring countries stretching from Ukraine in the west through Russia, Kazakhstan, Turkmenistan and Uzbekistan to the Altai, Koppet Dag and Tian Shan ranges in China. The Eurasian Steppe is speculatedbyDavid W. Anthony to have had a role in the spread of the horse, the wheel and Indo-European languages.[3] In the Eurasian steppe, soils often consist of chernozem.
The inner parts of AnatoliainTurkey, Central Anatolia and East Anatolia in particular and also some parts of Southeast Anatolia, as well as much of Armenia and Iran are largely dominated by cold steppe.
The Pannonian Plain is another steppe region in Central Europe, centered in Hungary but also including portions of Slovakia, Poland, Ukraine, Romania, Serbia, Croatia, Slovenia, and Austria. Another large steppe area (prairie) is located in the central United States, western Canada and the northern part of Mexico. The shortgrass prairie steppe is the westernmost part of the Great Plains region. The Columbia Plateau in southern British Columbia, Oregon, Idaho, and Washington state, is an example of a steppe region in North America outside of the Great Plains.
InSouth America, cold steppe can be found in Patagonia and much of the high elevation regions east of the southern Andes.
Relatively small steppe areas can be found in the interior of the South IslandofNew Zealand.
InAustralia, a moderately sized temperate steppe region exists in the northern and northwest regions of Victoria, extending to the southern and mid regions of New South Wales. This area borders the semi-arid and arid Australian Outback which is found farther inland on the continent.
InEurope, some Mediterranean areas have a steppe-like vegetation, such as central SicilyinItaly, southern Portugal, parts of Greece in the southern Athens area,[4] and central-eastern Spain, especially the southeastern coast (around Murcia), and places cut off from adequate moisture due to rain shadow effects such as Zaragoza.
In northern Africa, the Mediterranean area also hosts the same steppe-like vegetation, such as the Algerian-Moroccan Hautes Plaines and by extension the North Saharan steppe and woodlands.
InAsia, a subtropical steppe can be found in semi-arid lands that fringe the Thar Desert of the Indian subcontinent as well as much of the Deccan Plateau in the rain shadow of the Western Ghats, and the Badia of the Levant.
InAustralia, subtropical steppe can be found in a belt surrounding the most severe deserts of the continent and around the Musgrave Ranges.
InNorth America this environment is typical of transition areas between zones with a Mediterranean climate and true deserts, such as Reno, Nevada, the inner part of California, and much of western Texas and adjacent areas in Mexico.
There are many definitions of steppes. For example, Allan (1946) provides fifty-four definitions of this term. Stamp and Clark (1979) define steppes as 'mid-latitude areas dominated by herbaceous vegetation and termed locally steppes, prairies, pampas, high veldts, downland, etc.'
[...] the critical era when innovative Proto-Indo-European dialects began to spread across the steppes.
|
| |
|---|---|
| Physiognomy |
|
| Latitude |
|
| Climatic regime |
|
| Altitude |
|
| Leaves |
|
| Substrate |
|
| See also |
|
|
| |
|---|---|
| Mountainous |
|
| Continental plain |
|
| Fluvial |
|
| Glacial |
|
| Oceanic and coastal landforms |
|
| Volcanic |
|
| Aeolian |
|
| Artificial |
|
| |
| National |
|
|---|---|
| Other |
|
