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Meili Xue Shan (Chinese:梅里雪山, translation: "Mainri snowy range") or Mainri Snow Mountains (Tibetan: སྨན་རི།) is a mountain range in the Chinese province of Yunnan. It lies close to the northwestern boundary of the province and is bounded by the Salween River on the west and the Mekong on the east. The Meili are subrange of the larger Nu Mountains, themselves a constituent range of the Hengduan group.

Meili Snow Mountains
Highest point
PeakKawagebo
Elevation6,740 m (22,110 ft)
Coordinates28°26′14″N 98°41′04″E
Dimensions
Length200 km (120 mi) North-south
Width30 km (19 mi) East-west
Area6,000 km2 (2,300 sq mi)
Naming
Native name梅里雪山 (Chinese)
Geography
Meili Snow Mountains
CountryChina
StateYunnan
RiversSalween and Mekong
SettlementDeqen is the closest settlement of considerable size
Parent rangeHengduan Mountain

The crest of the range rises to over 6,000 metres (20,000 ft) above sea level, making for impressive prominence over the river valleys to the east and west, which are between 1,500 metres (4,900 ft) and 1,900 metres (6,200 ft) in elevation. The highest peak is Kawagarbo, which rises to 6,740 metres (22,110 ft). Kawagarbo is considered sacred for Tibetan Buddhists. Other significant peaks include Mianzimu, Cogar Laka and Jiariren-an. Because of restrictions and dangerous conditions, none of the major peaks in the range have ever been summited.


Name


In Tibet, people usually call the mountain by its peak Kawagarbo or Taizi(Prince) Snow Mountain.

In Tibetan, "Meili/Mainri" means mountains of herbs. People named the mountain "Meili/Mainri" because of the valuable herbs on this mountain.[1]


Main Peaks


Photo of Mianzimu
Photo of Mianzimu
Photo of Jiariren-an
Photo of Jiariren-an

Meili Snow mountain has 13 main peaks. They are also called "Taizi(Prince) Thirteen Peaks".


History



Expedition Records



The Prohibition of the Expedition


Kawagarbo(Meili Snow Mountain) is known as the sacred mountain in Tibetan Culture. The local people believe the climbing activities on the mountain is a blasphemy and the accidents that happened in the past is the anger of the gods. Considering from both the perspective of the local culture and the safety of the expedition, the local government has decided to stop climbing activities on Meili Snow Mountain.[2]


Climate



Temperature


The average temperature in Meili Snow Mountain Area has had a trend of increasing each year since 1990.[4]

The temperature of the area is distributed by the mountain range that splits the area into west and east. The temperature on the North-West side increases the most while the east remains mostly the same across the whole year. The increasing trend of temperature in the Meili Snow Mountain range has a strong correlation with the elevation. At an area higher than 4,000m, the temperature's increasing trend gets larger per meter. [4]


Precipitation


The precipitation has a huge trend of decreasing each year. Most of the precipitation is in summer while winter has the least.[4]

The monsoon period contributes the most to the annual precipitation. Approximately 67% of the precipitation is in the Monsoon period. Among all the observations since 1990, the precipitation in Spring has decreased by 10% in total. The amount of precipitation also has a strong correlation with the elevation. During the monsoon period, the precipitation decreases as the elevation gets lower on the west side of the mountain range. However, the precipitation raises tremendously on the east side of the mountain where the elevation is below 3,700m.[4]


Climate Change


Due to the increasing trend of temperature and the decreasing trend of precipitation, the Meili Snow Mountain range is facing a huge challenge that its glacier water resource is getting scarcer annually. Protecting the environment and preventing the area from losing its water resource becomes more important each year. The environmental protection in Meili Snow Mountain could be decisive to its biome system.[4]


References


  1. Chang jian Zang yu ren ming di ming ci dian = Dictionary of common Tibetan personal and place names. Guansheng Chen, Caidan An, 陈观胜., 安才旦. (Di 1 ban ed.). Beijing Shi: Wai wen chu ban she. 2004. ISBN 7-119-03497-9. OCLC 65173194.{{cite book}}: CS1 maint: others (link)
  2. Bairi setsuzan : Jūshichinin no tomo o sagashite. Naoyuki Kobayashi, 尚礼 小林. Tōkyō: Yama To Keikokusha. 2006. ISBN 4-635-28065-9. OCLC 675441024.{{cite book}}: CS1 maint: others (link)
  3. "AAC Publications - East of the Himalaya, Part II: Three Rivers Gorges of the Hengduan Mountains". publications.americanalpineclub.org. Retrieved 2022-10-06.
  4. Wen-Fei, Miao; Shi-Yin, L. I. U.; Yu, Z. H. U.; Shi-Mei, Duan; Feng-Ze, H. a. N. (2022-05-30). "Spatio-temporal differentiation and altitude dependence of temperature and precipitation in Meili Snow Mountains". Advances in Climate Change Research. 18 (3): 328. doi:10.12006/j.issn.1673-1719.2021.207. ISSN 1673-1719.

На других языках


- [en] Meili Snow Mountains

[fr] Monts Meili Xue

Les monts Meili Xue (tibétain : སྨན་རི།, Wylie : sman ri, THL : men ri (Mainri) ; chinois simplifié : 梅里雪山 ; pinyin : méilǐ xuěshān ; litt. « mont enneigée Meili ») sont un massif montagneux dont le point culminant est le Kawa Karpo culminant à 6 740 mètres d'altitude. Ils font partie des monts Hengduan, à la jonction entre le xian de Dêqên, préfecture autonome tibétaine de Dêqên, dans la province du Yunnan, et la région autonome du Tibet, en République populaire de Chine. Ils sont classés par l'office du tourisme chinois en catégorie AAAA.



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