Altun Shan National Nature Reserve

Altun Shan National Nature Reserve (simplified Chinese: 阿尔金山; traditional Chinese: 阿爾金山; pinyin: Ā'ěr jīnshān) (literally, “O You Golden Mountain”) 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 (no outlets to the sea) in the western third of the Altyn-Tagh mountains ("Altun Shan").[3] The reserve is sometimes referred to as the "Arjin Mountains Nature Reserve", or "Aerjinshan".[4] The reserve covers the southern portions of Qiemo County and Ruoqiang County (including Qimantag Township (祁曼塔格乡)) of Bayingolin Mongol Autonomous Prefecture in Xinjiang.

Altun Shan
National Nature Reserve
(also: Aerjinshan)
IUCN category IV (habitat/species management area)
Borders of Altun Shan Reserve (in Red)
Location, in Xinjiang Autonomous Region
LocationXinjiang Autonomous Region, China
Nearest cityRuoqiang Town, Ruoqiang County
Coordinates38.598°N 88.997°E / 38.598; 88.997[1]
Area1,512,500 ha (15,125 km2; 5,840 sq mi)
Established1983

Topography
Map including areas in the eastern part of the Altun Shan National Nature Reserve (1975)

The Altun Shan Reserve is an elongated triangular area on the southern edge of the Taklamakan Desert, just south of the Tarim Basin. The reserve occupies the "V"-shaped region between the southern slopes of the Altun Shan range on the north and the northern slopes of the Kulun mountain range on the south. The eastern third of the reserve is the Komkul Basin, an arid plateau at an altitude of 4,500 meters. The reserve measures about 800 km west-east, and 200 km north-south. There are no permanent towns or roads in the area.

There are three large lakes in the Kumkol basin of the reserve: Lake Ayakum, Lake Aqqikkal, and Lake Jingyu. All are saline ("salt lakes"). The northernmost, Lake Ayakum, is at an altitude of 12,685 feet and has an area of 283 sqmi. Its depth reaches 74 feet. To the west of Lake Ayakum is Lake Aqqikkal, at an altitude of 13,940 ft, and which is 16 miles across. Lake Jingyu is the southernmost.[5]

Climate

Because of its high altitude (over 4,500 meters above sea level) and arid location thousands of kilometers from any ocean and in the rain shadow of the Himalayas and other mountain, the climate of the reserve is "Cold desert climate" (Köppen climate classification "BWk" ). This climate is characterized by hot, dry summers, and very cold, dry winters. At the highest elevations, the climate is a Polar climate (Koppen "ET") with cooler summers but still cold and dry in the winter.

Ecoregion

Most of the reserve is in the "North Tibetan Plateau-Kunlun Mountains alpine desert" ecoregion, an area characterized by extreme aridity, high winds, and very cold winters.[6] The northeast of the reserve around Lake Ayakum is in the Qaidam Basin semi-desert ecoregion. Qaidam is the Mongolian word for 'salt', and the region is one of gravelly desert and some saline meadows and salt lakes.[7] Temperatures reach an average high of 56.5 °F (13.6 °C) in August, and average lows of −18.6 °F (−28.1 °C) in January. There is little to no precipitation in most years, but some frost cover.[7]

Flora and fauna

The reserve provides space outside of human development for some of the largest herds of hoofed in Asia: the vulnerable Tibetan wild yak (Bos mutus) (an estimated 10,000), wild ass (30,000), and Tibetan antelope (Pantholops hodgsonii) (up to 75,000).[8] The area is also an important habitat for the endangered Kozlov's Pika, and the relatively common Ladak pika.[9] There are also small populations of dholes (Wild Asiatic dogs).[10]

Access

Access is restricted, and high permit fees are required to enter. The soil is fragile and there are no permanent roads.

See also

References
  1. Er Jin Shan Nature Reserve protectedplanet.net
  2. Er Jin Shan Nature Reserve protectedplanet.net
  3. Mianping Zheng (1997). An Introduction to Saline Lakes on the Qinghai—Tibet Plateau. Springer Science & Business Media. pp. 21–. ISBN 978-0-7923-4098-0.
  4. "A Er Jin Shan". GlobalSpecies.org. Archived from the original on December 15, 2016. Retrieved October 1, 2016.
  5. Kum-kol Basin. The Encyclopædia Britannica: A Dictionary of Arts, Sciences, Literature and General Information. Encyclopædia Britannica Company. 1911. pp. 940–941.
  6. "North Tibetan Plateau-Kunlun Mountains alpine desert". Ecoregions of the World. GlobalSpecies.org. Archived from the original on 15 December 2016. Retrieved 8 October 2016.
  7. "Qaidam Basin semi-desert". Ecoregions of the World. GlobalSpecies.org. Archived from the original on 15 December 2016. Retrieved 8 October 2016.
  8. "China". Nature's Strpngholds. Nature's Strongholds Foundation. Archived from the original on 22 January 2015. Retrieved 3 October 2016.
  9. "Aerjinshan Nature Reserve". Protected Area Irreplacebility. Le Saout, S., Hoffmann, M., Shi, Y., Hughes, A., Bernard, C., Brooks, T.M., Bertzky, B., Butchart, S.H.M., Stuart, S.N., Badman, T., Rodrigues A.S.L. (2013) Protected areas and effective biodiversity conservation. Science 342: 803-805. Archived from the original on 15 December 2016. Retrieved 4 October 2016.
  10. Xue, Yadong; Li, Diqiang; Xiao, Wenfa; Zhang, Yuguang; Feng, Bin; Jia, Heng (2015). "Records of the dhole (Cuon alpinus) in an arid region of the Altun Mountains in western China". European Journal of Wildlife Research. 61 (6): 903–907. doi:10.1007/s10344-015-0947-z.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.