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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.
The Yarlung Tsangpo, also called Yarlung Zangbo (Tibetan: ཡར་ཀླུངས་གཙང་པོ་, Wylie: yar kLungs gTsang po, ZYPY: Yarlung Zangbo) and Yalu Zangbu River (Chinese: 雅鲁藏布江; pinyin: Yǎlǔzàngbù Jiāng) is a river that flows through the Tibet Autonomous Region of China and Arunachal Pradesh of India.
These effects of climate change endanger food security, freshwater access and global health. Climate change can be limited by using low-carbon energy sources such as wind and solar energy, by forestation, and shifts in agriculture. Adaptations such as coastline protection cannot by themselves avert the risk of severe, pervasive and irreversible ...
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).
A navbox on climate change Template parameters [Edit template data] Parameter Description Type Status (text) 1 Will expand a single section where appropriate Default all sections collapsed String optional (text) expanded Will expand a single section where appropriate Default all sections collapsed String optional (text) state Determines whether the navbox should be collapsed, expanded or ...
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.
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 ...
The climate is temperate semi-arid plateau monsoon, with most precipitation falling in the summer. Annual rainfall is 324.2 millimetres (12.76 in). [ 2 ] The average flow is 11.9 cubic metres per second (420 cu ft/s) per second, with least flow 4.6 cubic metres per second (160 cu ft/s) and flood flow rates of up to 400 cubic metres per second ...