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《Chinese Journal of Atmospheric Sciences》 2004-01
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On the Possibility of Ice Sheet over the Tibetan Plateau at the Last Glacial Maximum

Jiang Dabang, Wang Huijun, and Lang Xianmei(Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029) (State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
With the boundary conditions for the Last Glacial Maximum (LGM), the process-based equilibrium terrestrial biosphere model BIOME3 is used to simulate the potential paleovegetation distribution over China, and to detect the possibility of large-scale ice sheet over the Tibetan Plateau during the LGM. It turns out that vegetation distribution at the LGM is quite different from that at the present day, when the boreal temperate vegetation shift southward as a consequence of drier-colder climate compared to the present day. Sensitivity numerical experiments performed by BIOME3 also reveal that a large range of continental ice sheet do exist over the Qinghai-Xizang Plateau at the LGM.
【Fund】: 国家杰出青年基金 40 1 2 5 0 1 4;; 中国科学院知识创新工程重要方向性项目KZCX2 SW 1 3 3和KZCX2 1 0 8;; 中国科学院研究生科学与社会实践创新研究类项目共同资助
【CateGory Index】: P532
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