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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2011-04
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Analysis of the Surface Temperature over Keerqin Sand Aera in Inner Mongolia

ZHANG Peng1,ZHANG Hongsheng1,DU Jinlin1,LIU Huizhi2 1.Department of Atmospheric and Oceanic Sciences,School of Physics,Peking University,Beijing 100871;2.LAPC,Institute of Atmospheric Sciences,Chinese Sciences Academy,Beijing 100029  
Using the micrometeorological data obtained over the moving sand dune in Keerqin sand area in Inner Mongolia in summer of 2001 and spring of 2002,the surface temperature was determined and the characteristics were analyzed over the sand dune area.The idea is using discrete Fourier transform on the temperatures of different layers and applying soil heat conduction equation.The results are that soil temperature conductivity ratios which are calculated from the decline of the soil temperature amplitude and phase difference agree well under the assumption of layered homogeneity.The surface temperature was calculated using the relationship of the soil temperature conductivity ratios at different depths and the amplitude and phase of dominant and harmonic frequencies of soil temperature.The surface temperatures calculated from observed soil temperatures at 5 cm and 10 cm depth show a good agreement.The amplitude of soil temperature waves decreases exponentially with depth.The diurnal variation of soil temperature at 80 cm is small.
【Fund】: 国家自然科学基金(41075005);; 国家重点基础研究发展计划(2010CB428501);; 863计划(2006AA06A306);; 国家公益性行业(气象)科研专项基金(GYHY201006014)资助
【CateGory Index】: P423
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