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The response of lake change to climate fluctuation in north Qinghai-Tibet Plateau in last 30 years

Auteur(s) et Affiliation(s)

Tibet Inst. of Plateau Atmospheric and Environmental Science Research, Lhasa, Chine
Tibet Inst. of Plateau Atmospheric and Environmental Science Research, Lhasa, Chine
LI, L.
Tibet Inst. of Plateau Atmospheric and Environmental Science Research, Lhasa, Chine
WANG, W.
Tibet Inst. of Plateau Atmospheric and Environmental Science Research, Lhasa, Chine
Tibet Inst. of Plateau Atmospheric and Environmental Science Research, Lhasa, Chine


Description :
According to the analysis of the climate materials including the topographic map in 1975, the TM and CBERS satellite remote sensing materials from the 1980s to 2005 as well as the air temperature, precipitation, evaporation rate, maximum depth of snow and the biggest depth of frozen soil in the past 45 years, the water level area of 4 lakes at the south-east of Nagqu, Tibet including Bam Co, Pung Co, Dung Co and Nuripung Co show a distinct trend of expansion in the past 30 years. That is closely related to the warming and humidified climate change in the recent years such as rise of the air temperature, increase of the precipitation, decrease of the evaporation rate and permafrost degradation.


Type de document :
Article de périodique

Source :
Journal of geographical sciences. Acta geographica sinica, issn : 1009-637X, 2009, vol. 19, n°. 2, p. 131-142, nombre de pages : 12, Références bibliographiques : 16 ref.

Date :
2009

Editeur :
Pays édition : Chine

Langue :
Anglais
Droits :
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