【摘 要】
：
The Tibetan Plateau (TP) surfaces have been experiencing an overall rapid warming and wetting while wind speed and solar radiation have been declining in recent three decades.This study investigates h
【机 构】
：
Institute of Tibetan Plateau Research,CAS Cold an
【出 处】
：
第九届CTWF(CAS-TWAS-WMO)国际研讨会
论文部分内容阅读
The Tibetan Plateau (TP) surfaces have been experiencing an overall rapid warming and wetting while wind speed and solar radiation have been declining in recent three decades.This study investigates how climate changes influence the hydrological cycle in the TP during 1984-2006.To facilitate the analysis, a land surface model is used to simulate surface water budget at all CMA (China Meteorological Administration) stations in the TP.The simulated results are first validated against observed ground temperature and observation-derived heat flux in western TP and observed discharge trends in eastern TP.The response of evaporation and runoff to the climate changes is then analyzed.Major fmding are as follows.
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