证实利用地面水汽压资料可相当精确地计算出各地的可能太阳直接辐射日平均通量密度。
The results show that the daily average flux-density regime can be calculated quite accurately for various parts of the country by making use of the surface vapor pressure data.
高原效应的综合影响方面：地形抬升对地面感热通量的影响较小，对凝结潜热的影响明显。
For the integrated effects, the raising of TP has little influence on the surface sensible heat flux, while it greatly affects condensation heating.
结合辐射和土壤热通量观测资料揭示了两站的地面热量平衡状况，用地面热量平衡方程对以上结果进行了闭合误差检验。
The surface heat balance is discussed by involving the observational data of radiation and soil heat transfer, and the closed test of the surface heat balance equation is made.
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