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Multiplicative cascade models for fine spatial downscaling of rainfall: parameterization with rain gauge data

机译:精细级联降雨的乘积级联模型:使用雨量计数据进行参数化

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Capturing the spatial distribution of high-intensity rainfall overshort-time intervals is critical for accurately assessing the efficacy ofurban stormwater drainage systems. In a stochastic simulation framework, onemethod of generating realistic rainfall fields is by multiplicative randomcascade (MRC) models. Estimation of MRC model parameters has typicallyrelied on radar imagery or, less frequently, rainfall fields interpolatedfrom dense rain gauge networks. However, such data are not always available.Furthermore, the literature is lacking estimation procedures for spatiallyincomplete datasets. Therefore, we proposed a simple method of calibratingan MRC model when only data from a moderately dense network of rain gaugesis available, rather than from the full rainfall field. The number of gaugesneeds only be sufficient to adequately estimate the variance in the ratio ofthe rain rate at the rain gauges to the areal average rain rate across theentire spatial domain. In our example for Warsaw, Poland, we used 25 gaugesover an area of approximately 1600 km2. MRC models calibrated usingthe proposed method were used to downscale 15-min rainfall rates from a20 by 20 km area to the scale of the rain gauge capture area. Frequencydistributions of observed and simulated 15-min rainfall at the gaugescale were very similar. Moreover, the spatial covariance structure ofrainfall rates, as characterized by the semivariogram, was reproduced afterallowing the probability density function of the random cascade generator tovary with spatial scale.
机译:在短时间间隔内捕获高强度降雨的空间分布对于准确评估城市雨水排放系统的有效性至关重要。在随机模拟框架中,生成实际降雨场的一种方法是通过乘法随机级联(MRC)模型。 MRC模型参数的估计通常依赖于雷达图像,或者依赖于密集雨量仪网络内插的降雨场(频率较低)。但是,这样的数据并不总是可用。此外,文献缺乏空间不完整数据集的估计程序。因此,当只有来自中等密度雨量测量网络的数据而不是来自整个降雨场的数据可用时,我们提出了一种校准MRC模型的简单方法。仪表需求的数量仅足以充分估计整个空间域中雨表的降雨率与平均面积降雨率之比的方差。在波兰华沙的示例中,我们在大约1600 km 2 的面积上使用了25个仪表。使用所提出的方法校准的MRC模型用于将15分钟的降雨率从20分区域缩小到20公里以内的雨量计捕获区域。在标尺上观测到的和模拟的15分钟降雨的频率分布非常相似。此外,在允许随机级联生成器随空间尺度变化的概率密度函数之后,再现了以半变异函数为特征的降雨率的空间协方差结构。

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