The calculation of rainfall recharge amount is a very major content in mathematical (physical) analog calculation for ground or surface water.
在地下水和地表水的数学(物理)模拟计算中，降雨补给量的计算是非常重要的内容。
Although the water vapor convergence in the surface boundary layer is very important, the rainfall amount depends on the vertically integrated moisture flux convergence.
虽然边界层的水汽辐合对降水的形成很重要，但降水量的大小取决于整层水汽通量辐合的大小。
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