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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).
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.
Woka River Grade I Hydropower Station: built with the aid of China Development Bank. Langjiu Geothermal Power Station: financed by China Development Bank, Tibet Geothermal Development Company undertook the reconstruction of the power station. Lhasa West Suburb Transmission and Substation Project: invested and constructed by China Development Bank.
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).
The commissioning of the Qinghai-Tibet Networking Project has alleviated Tibet's energy bottleneck, fundamentally resolving its long-standing power supply issues. [3] The Qinghai-Tibet Networking Project is the world's highest-altitude and longest DC transmission line traversing permafrost regions.
Climate change can also be used more broadly to include changes to the climate that have happened throughout Earth's history. [32] Global warming—used as early as 1975 [33] —became the more popular term after NASA climate scientist James Hansen used it in his 1988 testimony in the U.S. Senate. [34] Since the 2000s, climate change has ...
WikiProject Climate change is a collaborative effort to improve our articles related to climate change.The WikiProject covers topics related to the causes of climatic change, the effects of climate change, and how society responds in terms of adaptation, mitigation and social and political change.
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 (14,000 cu ft/s).