North Tibetan Plateau–Kunlun Mountains alpine desert

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North Tibetan Plateau-Kunlun Mountains alpine desert
Kunlun IMG 0541.jpg
View of Western Kunlun Shan from the Tibet-Xinjiang highway
Ecoregion PA1011.png
Ecoregion territory (in purple)
Ecology
Realm Palearctic
Biome Montane grasslands and shrublands
Geography
Countries
Coordinates 35°45′N85°45′E / 35.750°N 85.750°E / 35.750; 85.750

The North Tibetan Plateau-Kunlun Mountains alpine desert ecoregion (WWF ID: PA1011) covers a long stretch of mostly treeless alpine terrain across the northern edge of the Tibet Plateau. A variety of cold, dry habitats are found, including alpine meadows, steppe, desert, and cushion plant floral areas. [1] [2]

Contents

Location

In the northwest, the ecoregion begins at the east edge of the Pamir Mountains, then covers the Kunlun Mountains in the north and the high plateau south to the Karakoram Mountains. From there it follows the Kunlun from west to east across the northern edge of the Tibet Plateau, on the south rim of the arid Tarim Basin. Elevations, higher in the northwest, are mostly above 5,000 meters, and the soils are often salty and barren. The region is dry, cold, and very remote. Permafrost lies under much of the territory. [1] Much of the eastern extension is within the Altun Shan National Nature Reserve.

Climate

The climate of the ecoregion is Tundra climate (Köppen climate classification ET), a local climate in which at least one month has an average temperature high enough to melt snow (0 °C (32 °F)), but no month with an average temperature in excess of 10 °C (50 °F). [3] [4] Precipitation in much of the region is under 50 mm/year. Winds are strong and persistent.

Flora and fauna

The harsh environment supports only specialized plants and animals capable of managing the cold, dry climate. There are very limited stands of Asian spruce ( Picea schrenkiana ) and juniper shrubs on low, north-facing slopes where they can capture moisture or snow melt. Along riverbeds there are a few plants such as a salt-tolerant form of tamarisk ( Myricaria ), a woody plant the exists mostly underground. Some slopes below 5,300 meters support a high cold steppe community that features sedges ( Carex ), purple feathergrass ( Stipa purpurea), falcate crazyweed (locoweed) ( Oxytropis falcata). [5]

One mammal endemic to the region is the endangered Koslov's pika (Ochotona koslowi). The Koslov's pika is a burrowing lagomorph that lives in dense family communities. The species had been identified in 1884 on the basis of two specimens, then 'lost' for over 100 years until scientists discovered some isolated communities in the Kunlun Mountains. [5]

Conservation

A 2017 estimate of the region approximated 239,046 square kilometers are included in protected areas, [6] including Chang Tang Nature Reserve, the world's third largest nature preserve; Sanjiangyuan; and Altun Shan National Nature Reserve. The Hoh Xil region in western Qinghai province was listed as a UNESCO World Heritage Site. [6]

See also

Related Research Articles

<span class="mw-page-title-main">Tibetan Plateau</span> Plateau in Central, South and East Asia

The Tibetan Plateau, also known as the Qinghai–Tibet Plateau or the Qing–Zang Plateau or as the Himalayan Plateau in India, is a vast elevated plateau located at the intersection of Central, South, and East Asia covering most of the Tibet Autonomous Region, most of Qinghai, western half of Sichuan, Southern Gansu provinces in Western China, southern Xinjiang, Bhutan, the Indian regions of Ladakh and Lahaul and Spiti as well as Gilgit-Baltistan in Pakistan, northwestern Nepal, eastern Tajikistan and southern Kyrgyzstan. It stretches approximately 1,000 kilometres (620 mi) north to south and 2,500 kilometres (1,600 mi) east to west. It is the world's highest and largest plateau above sea level, with an area of 2,500,000 square kilometres (970,000 sq mi). With an average elevation exceeding 4,500 metres (14,800 ft) and being surrounded by imposing mountain ranges that harbor the world's two highest summits, Mount Everest and K2, the Tibetan Plateau is often referred to as "the Roof of the World".

<span class="mw-page-title-main">Altun Shan National Nature Reserve</span>

Altun Shan National Nature Reserve is a large, arid area in the southeast of Xinjiang Autonomous Region, on the northern edge of the Tibetan plateau and the southern edge of the Tarim Basin in northwest China. It surrounds the Kumkol Basin, an endorheic basin in the western third of the Altyn-Tagh mountains. The reserve is sometimes referred to as the "Arjin Mountains Nature Reserve", or "Aerjinshan". The reserve covers the southern portions of Qiemo County and Ruoqiang County of Bayingolin Mongol Autonomous Prefecture in Xinjiang.

<span class="mw-page-title-main">Southeast Tibet shrub and meadows</span> Ecoregion in the Tibetan Plateau

The Southeast Tibet shrub and meadows are a montane grassland ecoregion that cover the southeast and eastern parts of the Tibetan Plateau in China. The meadows in this region of Tibet are in the path of the monsoon rains and are wetter than the other upland areas of the Tibetan Plateau. The "high cold" alpine terrain is one of high species diversity, due to the relatively high levels of precipitation for the region. Precipitation is lower in the northwest, and hence the vegetation thins from shrub to meadow or even desert.

<span class="mw-page-title-main">Altai montane forest and forest steppe</span> Ecoregion in the Altai Mountains

The Altai montane forest and forest steppe ecoregion covers patches of the subalpine forest belt on the Altai Mountains, crossing the border region where Russia, Kazakhstan, Mongolia and China meet. The region has high biodiversity, as it is located in transition zones between different ecoregions, altitudes, and climate zones. It is in the Palearctic realm, with a Cold semi-arid climate. It covers 35,199,998 km2 (13,590,795 sq mi).

<span class="mw-page-title-main">Altai alpine meadow and tundra</span> Ecoregion in the Altai Mountains

The Altai alpine meadow and tundra ecoregion is a terrestrial ecoregion covering the higher elevation of the Altai Mountains at the center of the "X" formed by the borders separating Russia, Kazakhstan, China, and Mongolia. The mountain peaks are the farthest north in Central Asia, separating the plains of Siberia to the north from the hot, dry deserts to the south. Altitudes above 2,400 meters display characteristics of tundra, with patches of alpine meadows and some trees immediately below the treeline. The ecoregion is in the montane grasslands and shrublands biome, and the Palearctic realm, with a humid continental climate. It covers an area of 90,132 square kilometres (34,800 sq mi).

<span class="mw-page-title-main">Qilian Mountains conifer forests</span> Ecoregion in the Tibetan Plateau

The Qilian Mountains Conifer Forests ecoregion is an ecoregion that consists of a series of isolated conifer forests on the northern slopes of the Qilian Mountain Range, on the northeast edge of the Tibetan Plateau in Qinghai and Gansu provinces of north-central China.

<span class="mw-page-title-main">Helanshan montane conifer forests</span> Ecoregion in the Helan Mountains

The Helanshan montane conifer forests ecoregion covers an isolated, forested mountain range surrounded by desert and semi-arid basins. As such, it has been called a "mountain island in the sky", and supports endemic species of plants and animals. The region supports the endangered Helan Shan pika.

<span class="mw-page-title-main">Tian Shan montane steppe and meadows</span>

The Tian Shan montane steppe and meadows ecoregion covers a 2,000 km long stretch of grasslands of the isolated Tian Shan mountains of Central Asia. It is characterized by high-altitude flat and rolling grasslands.

<span class="mw-page-title-main">Tian Shan foothill arid steppe</span> Ecoregion in the Tian Shan Mountains

The Tian Shan foothill arid steppe ecoregion covers the northern and western approaches to the Tian Shan mountains, centered on Lake Issyk-Kul in Kyrgyzstan. This region receives more moisture from Central Asia, thereby supporting more vegetation and diversity of plant and animal species than the deserts to the south.

<span class="mw-page-title-main">Pamir alpine desert and tundra</span> Ecoregion in the Pamir Mountains

The Pamir alpine desert and tundra ecoregion covers the high plateau of the Pamir Mountains, at the central meeting of the great mountain ranges of Central Asia: Himalaya, Karakoram, Hindu Kush, Kunlun, and Tian Shan. It is a region of relatively high biodiversity due to its central location and high elevation differentials, but it also acts as a barrier between the climate and habitats of north and south Asia.

<span class="mw-page-title-main">Central Tibetan Plateau alpine steppe</span> Ecoregion in the Tibetan Plateau

The Central Tibetan Plateau alpine steppe ecoregion covers the high alpine plateau that stretches over 1,600 kilometres (1,000 mi) across the Tibetan Plateau to Qinghai Lake in China. Because of the high altitude—much it over 5,000 metres (16,000 ft)—the region is a cold, arid desert that is only 20% covered with steppe and meadow vegetation. The area has been relatively free from human development due to the hostile climate and unsuitability for agriculture. The ecosystem is relatively intact, and supports herds of wild antelope, sheep, deer, and gazelles.

<span class="mw-page-title-main">Qilian Mountains subalpine meadows</span> Ecoregion in China

The Qilian Mountains subalpine meadows ecoregion covers the high meadows and shrubland of the Qilian Mountains, on the northeastern edge of the Tibetan Plateau in central China. These mountains form a divide between the dry regions of the Gobi Desert to the north, and the Qaidam Basin and the Tibetan Plateau to the south. While the habitat supports populations of marmots, grouse and some rare mammal species, the grasslands of the region are under pressure from over-grazing by domestic livestock.

<span class="mw-page-title-main">Tibetan Plateau alpine shrublands and meadows</span> Type of regional vegetation

The Tibetan Plateau alpine shrublands and meadows ecoregion covers the middle transition zone between the northern and southern regions of the Tibetan Plateau. The region supports both cold alpine steppe and meadows across a broad expanse of the plateau. Wild deer, antelope, and sheep roam the grasslands, but the habitat is increasingly being used to graze domestic livestock.

<span class="mw-page-title-main">Yarlung Tsangpo arid steppe</span> Ecoregion in the Tibetan Plateau

The Yarlung Tsangpo arid steppe ecoregion covers the river valley of the Yarlung Tsangpo River on the southern edge of Tibet. The river runs parallel to the northern borders of Nepal, Bhutan and India, between the Himalayas to the south and the Tibet Plateau to the north. The river valleys are the most populated areas of Tibet, putting pressure on wildlife. The area ranges from cold desert in the west to steppe shrub land in the east; the few trees are in the lowest river valleys to the east.

<span class="mw-page-title-main">Khangai Mountains alpine meadow</span> National park in Mongolia

The Khangai Mountains alpine meadows ecoregion runs along the central ridge of the Khangai Mountains in central Mongolia. The slopes to the north are conifer forests, the lowlands to the south are semi-arid steppe. The Khangai are an "island" mountain range surrounded by lower forest steppe and semi-arid regions of central Mongolia. Most of the region is now protected by Tarvagatai Nuruu National Park and Khangai Nuruu National Park.

<span class="mw-page-title-main">Central Asian riparian woodlands</span>

The Central Asian riparian woodlands ecoregion is spread out across the deserts and plains of central Asia between the Aral Sea and the mountains 2,000 kilometres (1,200 mi) to the east. The long narrow components of the ecoregion follow the large rivers fed by snowmelt, and provide critical habitat for migratory birds as they travel through the arid region. The vegetation is referred to as tugai, characterized by low tangles of trees and brush along the edges of the rivers and associated wetlands, and fed by groundwater instead of precipitation.

<span class="mw-page-title-main">Central Asian southern desert</span> Ecoregion

The Central Asian southern desert ecoregion is an arid but ecologically active region between the east coast of the Caspian Sea and steppes at the base of the mountains of central Asia. Most of Turkmenistan and eastern Uzbekistan is in this ecoregion. The winters are milder than in the cold desert to the north, and a large number of endemic species have adapted to living in the particular climate and soil of the region. As with sandy deserts in general, the region is notable for high numbers of endemic species of reptiles and insects.

<span class="mw-page-title-main">Kopet Dag woodlands and forest steppe</span>

The Kopet Dag woodlands and forest steppe ecoregion coincides with the Kopet Dag mountains, straddling the southern border of Turkmenistan and the northeastern border of Iran. The region is one of high biodiversity, as it includes a full range of altitude zones, and variety of habitats included juniper-wooded slopes, montane grasslands, and tugay.

<span class="mw-page-title-main">Gissaro–Alai open woodlands</span>

The Gissaro-Alai open woodlands ecoregion covers the western foothills winding around two western offshoots of the Tian Shan Mountains in western Tajikistan, and parts of eastern Uzbekistan and western Kyrgyzstan, in Central Asia. The woodlands are typically of Juniper trees and shrubs, fitting the altitude zone situated between the desert valley floor, and the tree line, above which the mountain ridges are glaciated and barren.

References

  1. 1 2 "North Tibetan Plateau-Kunlun Mountains alpine desert". Encyclopedia of the Earth. Retrieved March 9, 2020.
  2. "Map of Ecoregions 2017". Resolve, using WWF data. Retrieved September 14, 2019.
  3. Kottek, M.; Grieser, J.; Beck, C.; Rudolf, B.; Rubel, F. (2006). "World Map of Koppen-Geiger Climate Classification Updated" (PDF). Gebrüder Borntraeger 2006. Retrieved September 14, 2019.
  4. "Dataset - Koppen climate classifications". World Bank. Retrieved September 14, 2019.
  5. 1 2 Li, W.; Zhang, H.; Liu, Z. (2006). "Brief report on the status of Kozlov's pika, Ochotona koslowi (Büchner), in the east Kunlun mountains of China". Integrative Zoology. Integrative Zoology 2006; 1: 22-24. 1 (1): 22–4. doi: 10.1111/j.1749-4877.2006.00008.x . PMID   21395987.
  6. 1 2 Dinerstein, Eric [in German]; Olson, David; Joshi, Anup; Vynne, Carly; Burgess, Neil D.; Wikramanayake, Eric; Hahn, Nathan; Palminteri, Suzanne; Hedao, Prashant; Noss, Reed; Hansen, Matt; Locke, Harvey; Ellis, Erle C.; Jones, Benjamin; Barber, Charles Victor; Hayes, Randy; Kormos, Cyril; Martin, Vance; Crist, Eileen; Secrest, Wes; Price, Lori; Baillie, Jonathan E. M.; Weeden, Don; Suckling, Kierán; Davis, Crystal; Sizer, Nigel; Moore, Rebecca; Thau, Tanya; Potapov, Peter; Turubanova, Svetlana; Tyukavina, Alexandra; de Souza, Nadia; Pintea, Lilian; Brito, José C.; Llewellyn, Othman A.; Miller, Anthony G.; Patzelt, Annette; Ghazanfar, Shahina A.; Timberlate, Jonathan; Klöser, Heinz; Shennan-Farpón, Yara; Kindt, Roeland; Lillesø, Jens-Peter Barnekow; van Breugel, Paulo; Graudal, Lars; Voge, Maianna; Al-Shammari, Khalaf F.; Saleem, Muhammad (2017-04-05). "An Ecoregion-Based Approach to Protecting Half the Terrestrial Realm". BioScience . 67 (6): 534–545, Supplemental material 2 table S1b. doi: 10.1093/biosci/bix014 . ISSN   0006-3568. PMC   5451287 . PMID   28608869.