在试验过程中，主要考虑了4类模型：(1)后缘裂隙充水模型；(2)前缘洪水涨退模型；(3)坡面降水模型；(4)各种补给并存模型。

During the test, the four models were taken into account, (1) water filled in back fissures, (2) front flood fluctuation, (3) rain-fall on slope surface, and (4) combination of above three models.

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所有的模型都显示出对降水分布的影响。

All the models suggest some impact on the distribution of precipitation.

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但随着南极洲持续变暖，科里和刘继平的模型显示，雪变成了雨（见下图），总降水量上升了（见上图）。

But as the Antarctic continues to warm, Curry and Liu's models show snow becoming rain (see image below), even as total precipitation rises (see image above).

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