IHACRES模型
IHACRES是一个UH降水径流模型，它在集水处被汇集。集水储存的集水地降水指数sk被计算，它依赖于先前的降水量和集水地干旱度而0和1之间变化。0表明集水地是干旱的，目前的降水会产生有效雨量；1表明集水地是饱和的，目前的所以的降水会变成有效径流。
式中，c非线性存储的最大容积；rk是在第k时间段的实际降水；uk是有效降雨量；τw（tk)是温度tk时集水地烘干的时间常数。根据：
式中，τw是20℃时集水地烘干的时间常数；f是描述温度变化对烘干速率影响的因子。
有效雨量uk的计算如下：
Post DA，Jakeman AJ,Littlewood IG et al：水文反应中模拟地表下渗变化——Picaninny Creek，Victoria。Ecological Modelling，1996,86
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