Tibetanska visoravan
| Tibetanska visoravan | |
|---|---|
| 青藏高原 (Qīng–Zàng Gāoyuán, Ćinghaj–Tibetanska visoravan) | |
 | |
| Najviša tačka | |
| Najviša tačka | Tibetanska visoravan leži između himalajskog venca na jugu i pustinje Takla Makan na severu. (kompozitna slika) |
| Koordinate | 33° SGŠ; 88° IGD / 33° SGŠ; 88° IGD Koordinate: 33° SGŠ; 88° IGD / 33° SGŠ; 88° IGD |
| Dimenzije | |
| Dužina | 2500 km |
| Širina | 1000 km |
| Površina | 2500000 km2 |
| Geografija | |
 | |
| Države | Kina (Tibet, Ćinghaj, Zapadni Sičuan, Severni Junan, Južni Sinkjang, Zapadni Gansu) Indija (Ladak, Lahaul & Spiti), Pakistan (Gilgit Baltistan) Nepal (Severni Nepal) Butan Tadžikistan (Istočni Tadžikistan) Kirgistan (Južni Kirgistan) |
Tibetanska visoravan (tibetanski: བོད་ས་མཐོ།, Vajli: bod sa mtho), takođe poznata u Kini i kao Ćinghaj–tibetanska visoravan[1] ili Ćing–Cang visoravan[2] () ili kao Himalajska visoravan u Indiji,[3][4] je ogromna uzvišena visoravan u Centralnoj Aziji[5][6][7][8] i Istočnoj Aziji,[9][10][11][12] koja pokriva većinski deo Tibetanskog autonomnog regiona, Severozapadnog Junana, Zapadne polovine Sičuana, Južnog Gansua i Ćinghaj provincije u zapadnoj Kini, Indijske regione Ladak i Lahaul i Spiti (Himalajski Pradeđ) kao i Butan. Ova visoravan se proteže približno 1.000 km (620 mi) od severa do juga, i 2.500 km (1.600 mi) od istoka do zapada. To je najviša i najveća visoravan na svetu, sa površinom od 2.500.000 km2 (970.000 sq mi) (oko pet puta veličine Metropolitanske Francuske).[13] Njena prosečna elevacija nadmašuje 4.500 m (14.800 ft) i okružena je impozantnim planinskim lancima u kojima se nalaze dva najviša svetska vrha, Mont Everest i K2. Tibetanska visoravan se često naziva „krovom sveta”.
Tibetanska visoravan sadrži izvorišta slivova većine tokova u okolnim regionima. Njegove desetine hiljada glečera i drugih geografskih i ekoloških karakteristika služe kao „vodeni toranj” koji čuva vodu i održava protok. Ponekad se naziva i Trećim polom s obzirom na to da njegova ledena polja sadrže najveću rezervu sveže vode izvan polarnih područja. Uticaj globalnog zagrevanja na Tibetansku visoravan je od velikog naučnog interesa.[14][15][16][17]
Reference
[уреди | уреди извор]- ^ Wang, Zhaoyin; Li, Zhiwei; Xu, Mengzhen; Yu, Guoan (30. 3. 2016). River Morphodynamics and Stream Ecology of the Qinghai-Tibet Plateau. CRC Press.
- ^ Jones, J.A.; Liu, Changming; Woo, Ming-Ko; Kung, Hsiang-Te (6. 12. 2012). Regional Hydrological Response to Climate Change. Springer Science & Business Media. стр. 360.
- ^ „हिमालयी क्षेत्र में जीवन यापन पर रिसर्च करेंगे अमेरिका और भारत”. Amar Ujala (на језику: хинди). Приступљено 2023-07-25.
- ^ „In Little Tibet, a story of how displaced people rebuilt life in a distant land”. 18. 2. 2020.
- ^ Illustrated Atlas of the World (1986) Rand McNally & Company. ISBN 0-528-83190-9 pp. 164–65
- ^ Atlas of World History (1998 ) HarperCollins. ISBN 0-7230-1025-0 p. 39
- ^ „The Tibetan Empire in Central Asia (Christopher Beckwith)”. Приступљено 19. 2. 2009.
- ^ Hopkirk 1983, стр. 1
- ^ Peregrine, Peter Neal & Melvin Ember, etc. (2001). Encyclopedia of Prehistory: East Asia and Oceania, Volume 3. Springer. стр. 32. ISBN 978-0-306-46257-3.
- ^ Morris, Neil (2007). North and East Asia. Heinemann-Raintree Library. стр. 11. ISBN 978-1-4034-9898-4.
- ^ Webb, Andrew Alexander Gordon (2007). Contractional and Extensional Tectonics During the India-Asia Collision. ProQuest LLC. стр. 137. ISBN 978-0-549-50627-0.
- ^ Marston, Sallie A.; Paul L. Knox; Diana M. Liverman (2002). World regions in global context: peoples, places, and environments
. Prentice Hall. стр. 430. ISBN 978-0-13-022484-2.
- ^ „Natural World: Deserts”. National Geographic. Архивирано из оригинала 12. 1. 2006. г.
- ^ Leslie Hook (30. 8. 2013). „Tibet: life on the climate front line”. Financial Times. Приступљено 1. 9. 2013.
- ^ Liu, Xiaodong; Chen (2000). „Climatic warming in the Tibetan Plateau during recent decades”. International Journal of Climatology. 20 (14): 1729—1742. Bibcode:2000IJCli..20.1729L. CiteSeerX 10.1.1.669.5900
. doi:10.1002/1097-0088(20001130)20:14<1729::aid-joc556>3.0.co;2-y — преко Academia.edu.
- ^ Ni, Jian (2000). „A Simulation of Biomes on the Tibetan Plateau and Their Responses to Global Climate Change”. Mountain Research and Development. 20 (1): 80—89. doi:10.1659/0276-4741(2000)020[0080:ASOBOT]2.0.CO;2.
- ^ Cheng, Guodong; Wu (8. 6. 2007). „Responses of permafrost to climate change and their environmental significance, Qinghai-Tibet Plateau”. Journal of Geophysical Research. 112 (F2): F02S03. Bibcode:2007JGRF..112.2S03C. S2CID 14450823. doi:10.1029/2006JF000631.
Literatura
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Spoljašnje veze
[уреди | уреди извор]
- ON THINNER ICE 如履薄冰 (by GRIP, Asia Society and MediaStorm)
- The Third Pole: Understanding Asia's Water Crisis
- „The End of Earth's Summer”. Архивирано из оригинала 24. 07. 2002. г.
- Long Rivers and Distant Sources
- „"Roof of the Earth" Offers Clues About How Our Planet Was Shaped”. Архивирано из оригинала 31. 10. 2012. г.
- Plateau Perspectives (international NGO)
- „Leaf morphology and the timing of the rise of the Tibetan Plateau”. Архивирано из оригинала 21. 07. 2003. г.
- „Protected areas of the Tibetan Plateau region”. Архивирано из оригинала 10. 05. 2007. г.
- „North Tibetan Plateau-Kunlun Mountains alpine desert”. Terrestrial Ecoregions. World Wildlife Fund.
- Photos of Tibetan nomads
- „"Roof of the Earth" Offers Clues About How Our Planet Was Shaped”. Архивирано из оригинала 01. 05. 1997. г.
- „Contemporary lifestyle and language learning center from Tibet lhasa, the official language of Tibetan. podcast.”. Архивирано из оригинала 01. 02. 2015. г.
- Tibetan History-The true history of any region cannot be fully understood without knowing the basic characteristics of a region and of its inhabitants
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