The second is the process of water condensation determined by air vapor, soil surface temperature and the available energy of soil.
第二阶段是由近地面微气象条件决定的水分凝结过程，所吸收水量受空气水汽压、地面温度和地表可利用能量的影响。
The day change of soil surface temperature is obvious, having an obvious apogee, but the soil temperature of other depths, particularly the deep soil, temperature variety is not obvious.
林内外地表温度日变化明显，有一个明显的最高点，而其他深度的土壤温度，尤其是深层土壤温度变化则不明显。
It is showed that the forest can not only increase net radiation but also decrease sensible and soil heat fluxes by decreasing surface reflectance and temperature.
这表明森林通过降低地表反射率和表面温度，不仅增加地表净辐射，而且减少其用于感热和土壤热通量的消耗。
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