This kind of circulation directly influences the sub-grid surface fluxes.
这种环流的存在直接影响到次网格地表通量的计算。
In the known land surface model BATS, the calculations of the surface fluxes just depend on simple empirical formulae. These calculations are very sketchy.
在原有的陆面过程模式BATS中，对地表通量的计算基于简单的经验公式，这个计算是十分粗略的。
In addition to changes in temperatures and surface heat fluxes, they also observed changes in large-scale precipitation, particularly at the mid-latitudes in the Northern Hemisphere.
除了气温变化和地表的热传递，他们还观察到大规模的降水，特别是在北半球的中纬度地区。
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