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Yamdrok Lake. The geography of Tibet consists of the high mountains, lakes and rivers lying between Central, East and South Asia.Traditionally, Western (European and American) sources have regarded Tibet as being in Central Asia, though today's maps show a trend toward considering all of modern China, including Tibet, to be part of East Asia.
Earthquakes are common. The river basin is the center of Tibet politically, economically and culturally. As of 1990 the population was 329,700, of whom 208,700 were farmers. 88% of the people were ethnic Tibetans. [2] The climate is semi-arid monsoon, with a low average temperature of 1.2 to 7.5 °C (34.2 to 45.5 °F).
Major tributaries of Yarlung Tsangpo include Nyangchu River, Lhasa River, Nyang River, and Parlung Tsangpo. In Tibet the river flows through the South Tibet Valley, which is approximately 1,200 kilometres (750 mi) long and 300 kilometres (190 mi) wide. The valley descends from 4,500 metres (14,800 ft) above sea level to 3,000 metres (9,800 ft).
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. [1] [2] 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 ...
Climate Change on the Tibetan Plateau, Asia Society; Case Western Reserve University's Center for the Research on Tibet, a good source of downloadable articles about Tibetan nomads; Information on Qinghai and the SNNR, Plateau Perspectives; A Google Earth kmz file of the Sanjiangyuan Area, download from the World Database On Protected Areas
The Tibetan Plateau, [a] also known as Qinghai–Tibet Plateau [b] and Qing–Zang Plateau, [c] is a vast elevated plateau located at the intersection of Central, South, and East Asia. [ d ] Geographically, it is located to the north of Himalayas and the Indian subcontinent , and to the south of Tarim Basin and Mongolian Plateau .
Sog County has a dry-winter alpine subarctic climate (Köppen Dwc) with mild, rainy summers and freezing to frigid, dry winters with large diurnal temperature variations. Climate data for Sogxian, elevation 4,023 m (13,199 ft), (1991–2020 normals)
The Nyamjang Chu, [2] or Nyashang Chu [3] (Tibetan: ཉ་བཤང་ཆུ, Wylie: nya bshang chu, THL: nya shang chu) [4] [a] is a cross-border perennial river that originates in the Shannan Prefecture of Tibet and flows into the Arunachal Pradesh state of India, joining the Tawang Chu river just before it enters Bhutan.
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