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。
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.
与潜热的湍流输送及海表面向上的长波辐射通量相比，感热的湍流输送量很小。
Comparing with the flux of turbulent exchange of latent heat and the flux of upward long-wave radiation the flux of sensible heat exchange is very small.
文中集中分析了表面感热和潜热通量的时空分布特征。
Special attention is paid to the diagnosis of the temporal and spatial distributions of surface sensible and latent heat fluxes.
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