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  2. Tibetan Plateau - Wikipedia

    en.wikipedia.org/wiki/Tibetan_Plateau

    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 South, Central, 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 .

  3. Geography of Tibet - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Tibet

    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.

  4. Monsoon of South Asia - Wikipedia

    en.wikipedia.org/wiki/Monsoon_of_South_Asia

    This results in the north-to-south flow of the winds in the form of the northeast monsoon. With the northward shift of the vertical sun, this jet shifts north, too. The intense heat over the Tibetan Plateau, coupled with associated terrain features like the high altitude of the plateau, generate the tropical easterly jet over central India.

  5. Lhasa River - Wikipedia

    en.wikipedia.org/wiki/Lhasa_River

    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).

  6. Monsoon - Wikipedia

    en.wikipedia.org/wiki/Monsoon

    The limits of the ITCZ vary according to the land–sea heating contrast and it is thought that the northern extent of the monsoon in South Asia is influenced by the high Tibetan Plateau. [ 33 ] [ 34 ] These temperature imbalances happen because oceans and land absorb heat in different ways.

  7. Changtang - Wikipedia

    en.wikipedia.org/wiki/Changtang

    The Changtang Nature Reserve Map including part of the Changtang (labeled as CHANG-THANG) (DMA, 1975). Most of the Tibetan Changtang is now protected nature reserves consisting of the Chang Tang Nature Reserve, the second-largest nature reserve in the world, and four new adjoining smaller reserves totaling 496,000 square kilometres (192,000 sq mi) of connected nature reserves that represent an ...

  8. Tso Moriri - Wikipedia

    en.wikipedia.org/wiki/Tso_Moriri

    Tso Moriri frozen Buddhist shrine.On the banks of Tso Moriri, Leh district, Ladkah, 2010 Lake Tsomoriri and sign.. Tso Moriri or Lake Moriri (Tibetan: ལྷ་མོའི་བླ་མཚོ, Wylie: lha mo bla mtsho) or "Mountain Lake", is a lake in the Changthang Plateau (literally: northern plains) in Leh district of the union territory of Ladakh in India.

  9. Jiuzhaigou - Wikipedia

    en.wikipedia.org/wiki/Jiuzhaigou

    The climate is subtropical to temperate monsoon with a mean annual temperature of 7.8 °C, with means of −3.7 °C in January and 16.8 °C in July. [4] Total annual rainfall is 761 mm but in the cloud forest it is at least 1,000 mm. [ 4 ] 80% of rainfall occurs between May and October. [ 4 ]