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Precipitation variability in central Himalayas and its relation to Northern Hemisphere temperature
A 149.8-m-long ice core was drilled at the accumulation area of Dasuopu glacier (28°23′N, 85°43′E, 7100 m a.s.l.) in the central Himalayas in 1997. The ice core was analyzed continuously for stable isotopes (δ18O), cations (Na+, K+, Mg2+, Ca2+) and anions (Cl-,SO2-4,NO3-) throughout the core. Cycles indicated by δ18O, cations and anions were identified and counted as seasonal fluctuations as annual increment from maximum to maximum values. Reconstructed 300-year annual net accumulation from the core reveals a major precipitation trend for the central Himalayas with an average precipitation 750 mm per year. The trend, separated from the time series, shows a strong correlation to global temperature. Generally, as northern global temperature increases 0.1℃, the accumulation decreases about 80mm and vise versa. This may suggests that monsoon precipitation in Himalayas have decreased continuously in past decade as a response to global warming.
作 者： DUAN Keqin YAO Tandong 作者單位： DUAN Keqin(Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy Sciences, Lanzhou 730000, China;National Laboratory of Western China's Environmental Systems, Lanzhou University, Lanzhou 730000, China)YAO Tandong(Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy Sciences, Lanzhou 730000, China)
刊 名： 科學通報(英文版) SCI 英文刊名： CHINESE SCIENCE BULLETIN 年，卷(期)： 2003 48(14) 分類號： X14 關鍵詞： monsoon precipitation Himalayas global warming