地表热量平衡
- 网络surface energy balance
地表热量平衡-
蒸发是地表热量平衡和水量平衡的组成部分，是水循环中最直接受土地利用和气候变化影响的一项。
Evaporation is an important component of the hydrologic cycle and the climate change .
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结果表明，本模式能合理地模拟荒漠下垫面地表热量平衡、土壤体积含水量、地表植被蒸发散阻抗、地表水汽通量日变化和湍流交换系数、湍流动能、位温和比湿廓线等。
The results show that this model can reasonably simulate the diurnal variations of heat balance , soil volumetric water content , resistance of vegetation evaporation , flux of surface moisture , and profiles of turbulent exchange coefficient , turbulent momentum , potential temperature , and humidity mixing ratio .
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敦煌地区荒漠戈壁地表热量和辐射平衡特征的研究
The Influence of Synoptic Conditions on the Averaged Surface Heat and Radiation Budget Energy over Desert or Gobi