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Copula-based downscaling of spatial rainfall: a proof of concept

机译:基于Copula的空间降雨缩减:概念验证

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Fine-scale rainfall data is important for many hydrological applications.However, often the only data available is at a coarse scale. To bridge thisgap in resolution, stochastic disaggregation methods can be used. Suchmethods generally assume that the distribution of the field is stationary,i.e. the distribution for the entire (fine-scale) field is the same as thedistribution of a smaller region within the field. This assumption isgenerally incorrect and we provide a proof of concept of a method to estimatethe distribution of a smaller region. In this method, a copula is used toconstruct a bivariate distribution describing the relation between thescales. This distribution is then used to estimate the distribution of thefine-scale rainfall within a single coarse-scale pixel, by conditioning onthe coarse-scale rainfall depth.
机译:精细尺度的降雨数据对于许多水文应用都很重要,但是,通常唯一可用的数据是粗略的。为了缩小分辨率之间的差距,可以使用随机分解方法。这样的方法通常假定场的分布是固定的,即。整个(精细尺度)场的分布与场内较小区域的分布相同。这种假设通常是不正确的,我们提供了一种估计较小区域分布的方法的概念证明。在这种方法中,系动词被用于构造描述尺度之间关系的双变量分布。然后,通过以粗雨量深度为条件,此分布可用于估计单个粗雨量像素内的小雨量分布。

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