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《Journal of Glaciology and Geocryology》 2005-05
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Seasonal Variation on Land Surface Energy Budget and Energy Balance Components in the Northern Tibetan Plateau

MA Wei-qiang~(1,2),\ MA Yao-ming~(1,3),\ LI Mao-shan~(1,2),\ Z.(Bob) SU~(4),\ WANG Jie-min~(1) (1.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China;2.Key Laboratory of Regional Climate-Environment Research for Template East Asia(RCE-TEA),Chinese Academy of Sciences,Beijing 100039,China;3.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China;4.Spatial Hydrology and Water Resources Management International Institute for Geo-Information Science and Earth Observation(ITC),Hengelosestraat 99,P.O.Box 6 7500 AA Enschede,The Netherlands)  
It is very important to study the regional heat fluxes in the Tibetan Plateau Area.Using CAMP/Tibet(CEOP,Coordinated Enhanced Observing Period) Asia-Australia Monsoon Project(CAMP) on the Tibetan Plateau(CAMP/Tibet,2001-2005)) data,land surface heat fluxes are analyzed.Those are the net radiation flux(R_(n))、sensible heat fluxes(H)、latent heat fluxes((E) and soil heat fluxes(G_(0)).Some new results are gotten in the Northern Tibetan Plateau.1) In the Tibet plateau,the yearly variations of downward shortwave and long-wave radiation,upward shortwave and long-wave radiation,net radiation fluxes are clearly,its July numerical values are larger than January.Their eigenvalueas are 230,245,53,345 and 95 W\5m~(-2);2) In the Tibetan Plateau,the diurnal variations of net radiation,sensible,latent and soil heat fluxes are clearly.They increase with the increasing of solar altitude angle after the sunrise in the morning,and the maximum appears around the noon then they decrease with the decreasing of solar altitude angle.3) Latent heat flux is the main point in summer and sensible heat flux is the main point in winter.In June latent heat flux and sensible heat flux is almost equality.At the beginning of July the latent heat flux is the main aspect until September,then sensible heat flux is the main aspect until the coming year if May.4) The variation of soil heat flux is slow and its value is very small.
【Fund】: 中国科学院大气物理研究所东亚区域气候环境重点实验室2005年开放课题项目;; 中国科学院知识创新工程方向性项目(KZCX3-SW-329KZCX3-SW-339)资助
【CateGory Index】: P422.4
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