Using the modified MASS model and terrain data of Liaoning, the effect of terrain on diurnal variation of the wind field in the ground layer is simulated.
利用修改的Mass模式和辽宁地区的地形资料，模拟了地形加热作用对辽宁地区近地层风场日变化的影响。
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And decreases in diurnal temperature range and wind speed were found to be the main influencing factors leading to the decrease of pan evaporation.