Modification of the land surface energy balance relationship by introducing vertical sensible heat advection and soil heat storage over the Loess Plateau

查看全文 作　　者：ZHANG [1,2,3]Qiang;LI [3,1]HongYu;ZHAO [1,3]JianHua

机构地区：[1]Key laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province,Key Open Laboratory of Arid Climatic Change and Disaster Reduction,Institute of Arid Meteorology,China Meteorological Administration,Lanzhou 730020,China;[2]Gansu Provincial Meteorological Bureau,Lanzhou 730020,China;[3]College of Atmospheric Sciences,Lanzhou University,Lanzhou 730000,China

出　　处：《Science China Earth Sciences》索引2012年第55卷第4期,共10页

基　　金：supported by the National Natural Science Foundation of China (Grant No.40830597);the Public Welfare Research Project of China (Grant No.GYHY200806021) 摘　　要：Little is known about the surface energy balance problem for a complex underlying surface.Taking data from the Loess Plateau Land-surface Processes Experiment(LOPEX) and investigating the characteristics of the surface energy balance over a complex underlying surface,this paper calculates the soil heat storage and vertical sensible heat advection,analyzes their contributions to the surface energy imbalance,and discusses the mechanism by which the vertical velocity and temperature gradient in the surface layer affect the vertical sensible heat advection transfer.We found that the vertical velocity in the surface layer provides the necessary dynamic power for vertical sensible heat advection,and a relatively strong temperature gradient is the energy source generating vertical sensible heat advection.Under an ascending condition,the effect of vertical sensible heat advection on the surface energy budget is more obvious.It is also found that when the soil heat storage term and the vertical sensible heat advection term are added to the energy balance equation,the imbalance significantly improves.The peak of average diurnal residuals decreases from 125.1 to 41.5 W m-2,the daily average absolute value of residuals falls from 59.0 to 26.4 W m-2,and the surface energy balance closure increases from 78.4% to 94.0%. 关键词：地表能量平衡垂直速度黄土高原热平流平衡关系土壤能量不平衡残差绝对值

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Modification of the land surface energy balance relationship by introducing vertical sensible heat advection and soil heat storage over the Loess Plateau

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