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首页> 外文期刊>Journal of hydrometeorology >Satellite Rainfall Estimates for Debris Flow Prediction: An Evaluation Based on Rainfall Accumulation-Duration Thresholds
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Satellite Rainfall Estimates for Debris Flow Prediction: An Evaluation Based on Rainfall Accumulation-Duration Thresholds

机译:用于碎片流量预测的卫星降雨估计:基于降雨累积持续时间阈值的评估

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摘要

Rainfall thresholds are often used in early warning systems to identify rainfall conditions that, when reached or exceeded, are likely to result in debris flows. Rain gauges are typically used for the definition of these thresholds. However, in mountainous areas in situ observations are often sparse or nonexistent. Satellite-based rainfall estimates offer a solution to overcome the coverage problem at the global scale but are associated with significant estimation uncertainty. Evaluating satellite-based rainfall thresholds is thus necessary to understand their potential and limitations. In this work, an intercomparison among satellite-based precipitation products is presented in the context of estimating rainfall thresholds for debris flow prediction. The study is performed for the upper Adige River basin in the eastern Italian Alps during 2000-10. Large differences are observed between event-based characteristics (event duration and magnitude) derived from rain gauge and satellite-based estimates, revealing considerable interproduct variability in the debris flow-triggering rainfall characteristics. The parameters of the satellite-based thresholds differ less than 30% from the corresponding rain gauge-based parameters. Results further suggest that the adjustment of satellite-based estimates (either gauge based or by applying an error model) together with spatial resolution has an important impact on the estimation of the accumulation-duration thresholds.
机译:降雨阈值通常用于预警系统,以确定达到或超过时可能导致泥石流的降雨条件。雨量计通常用于定义这些阈值。然而,在山区,现场观测往往很少或根本不存在。基于卫星的降雨估算为克服全球范围的覆盖问题提供了一种解决方案,但与重大的估算不确定性有关。因此,有必要评估卫星降雨阈值,以了解其潜力和局限性。在这项工作中,基于卫星的降水产品之间的相互比较是在估算泥石流预测降雨阈值的背景下进行的。这项研究是在2000年至2010年期间对意大利东部阿尔卑斯山的阿迪奇河上游流域进行的。根据雨量计得出的基于事件的特征(事件持续时间和量级)与基于卫星的估计之间存在很大差异,这表明触发降雨特征的泥石流具有相当大的产品间可变性。基于卫星的阈值参数与相应的基于雨量计的参数相差不到30%。结果进一步表明,基于卫星的估计(基于量表或通过应用误差模型)以及空间分辨率的调整对累积持续时间阈值的估计有重要影响。

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