Simulation of freezing and melting of soil on the northeast Tibetan Plateau

查看全文 作　　者：XIA Kun 1,2,3,LUO Yong 2,4,5 & LI WeiPing 2 1 Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China;2National Climate Center,China Meteorological Administration,Beijing 100081,China;3Graduate University of Chinese Academy of Sciences,Beijing 100049,China;4 Center for Earth System Science,Tsinghua University,Beijing 100084,China;5Key Laboratory of Earth System Numerical Simulation,Ministry of Education,Beijing 100084,China

出　　处：《Chinese Science Bulletin》索引2011年第56卷第20期,共11页

基　　金：supported by the National Basic Research Program of China(2007CB411505);the Major National Scientific Research Project on Global Changes(2010CB951902);the National Natural Science Foundation of China(40975042 and 40905046) 摘　　要：Using observational data spanning the period from February to December 2009 and recorded at the Suli station in Qinghai Province,the land-surface model CLM3.0 was employed to simulate the freezing and melting of soil.The results indicate that the simulated soil temperature is higher than the observed soil temperature and the ultimate thawing date is earlier than the observed date during the melting period.During the freezing period,the simulated soil temperature is lower than the observed soil temperature and the ultimate freezing of the deep soil is earlier than that observed.Overall,the simulation of freezing is better than that of melting,and the simulation of a shallow layer is better than that of a deeper layer.In the original CLM3.0,it is assumed that frozen soil begins to melt when the soil temperature exceeds 0C,which is inconsistent with observations.The critical freeze-thaw temperature was calculated according to thermodynamics equations and the freeze-thaw condition was modified.In this work,the melting rate for frozen soil was reduced using the modified scheme,and the simulated soil temperature was lowered. Meanwhile,the refreezing of soil during the melting season was well simulated and more closely matched observations.Additionally,it was found that the rates of melting and freezing differ,with the former being slower than the latter,but refreezing during the melting season is rather quick. 关键词：土壤温度冻结期青藏高原东北部模拟融化观测数据热力学方程表面模型

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Simulation of freezing and melting of soil on the northeast Tibetan Plateau

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