考虑了降水分布的次网格特征及其对陆面水文产生的重要影响。

In the land surface hydrological processes, the subgrid distribution of precipitation and its effects are taken into account.

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地面气象要素的次网格分布是产生区域通量计算误差的主要原因之一。

One of the primary reason that caused the grid-scale flux deviation between model results and reality is the nonhomogeneous distribution of the land surface meteorology parameters.

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二次细分网格位移边界值采用等参逆变换法由一次网格的计算结果插值得到。

The displacement boundary values of the small model use the results of the large model, which are obtained by interpolating with numerical inverse isoparametric mapping.

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