supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-145);the Global Change Research Program of China (2010CB951401);the National Natural Science Foundation of China (40830743)
During the summer monsoon season,the moisture of precipitation events in southern and central regions of the Tibetan Plateau is mainly moisture from the Indian Ocean transported by the Indian monsoon and terrestrial v...
supported by the National Natural Science Foundation of China(40903050and 40830743);the National Basic Research Program of China(2005CB422004);the State Key Laboratory of Cryospheric Sciences(SKLCS-ZZ-2008-01 and SKLCS09-06)
The Yarlung Zangbo River is the highest river in the world.It flows from west to east through the southern part of Tibet.The mercury(Hg)speciation and distribution in surface waters and soils near the bank of the Yarl...
supported by the National Basic Research Program of China (2005CB422004);the National Natural Science Foundation of China (40830743,40605034 and 40771187);the Foundation of State Key Laboratory of Cryospheric Science,Chinese Academy of Sciences (SKLCS-ZZ-2008-01)
Thirty samples of total suspended particles were collected at a site in western part of Lhasa,Tibet from August 2006 to July 2007.The 10Be concentrations were determined by Accelerator Mass Spectrometer (AMS).Analysis...
supported by the National Natural Science Foundation of China(40971050,40830743 and 40671045);the Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-YW-145,317);the National Basic Research Program of China(2005CB422004)
This paper describes 2007/2008 inter-annual changes in runoff from the Zhadang Glacier located on the northern slope of Nyainqêntanglha Range,Tibet,and analyzes their causes.Precipitation increased by 17.9%in summer ...