还以实际降水数据检验了降水强度的指数分布，在此基础上求出了模型的解。

Then based on the exponential distribution of precipitation the model was solved to give the equivalent precipitation of each level in the landscape.

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本文从熵极大原理出发导出了在一次降水过程中降水强度与其历时为负指数关系。

Under a very simple constrain from the Maximum Entropy Principle, we found that an intensity-duration relation of Precipatation processes obeys negative exponent law.

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