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《JOURNAL OF GLACIOLGY AND GEOCRYOLOGY》 1995-02
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Studies on Altitude and Climatic Environment in the Middle and East Parts of Tibetan Plateau during Quaternary Maximum Glaciation

Shi Yafeng; Zheng Benxing; Li Shijie and Ye Baisheng(Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences, 730000)  
A wide variety of informations is used in this paper to comprehensively infer the altitude and climatic environment during Quaternary maximum glaciation. It is suggested that the time of Quaternary maximum glaciation appearance is in correspondence with the deep sea core oxygen isotopic stages 18-16(0.72-0.52MaBP). At that time the height of the Plateau was approximately 1000 m lower than that at present, the total glacierized area of four major mountain ranges (Tanggula, A'nyemaqen, Golog and Daocheng Haizi) in the middle and east parts of the plateau was 40000km ̄2, 18 times larger than that at present, the eqilibrium line altitude varied from 3450 to 4250 m, the average air temperature from June to August varied from 2.3 to 3.4℃ , and the annual precipitation varied between 1260 and 1960 mm, 1.8to 3.2 times more than that at present at the equilibrium line altitude.
【Fund】: 国家自然科学基金 国家八五攀登计划青藏项目
【CateGory Index】: P532
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