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Precipitation Forecasting with Gamma Distribution Models for Gridded Precipitation Events in Eastern Oklahoma and Northwestern Arkansas

机译:俄克拉荷马州东部和阿肯色州西北部的网格化降水事件的伽马分布模型进行降水预报。

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摘要

An elegant and easy to implement probabilistic quantitative precipitation forecasting model that can be used to estimate the probability of exceedance (POE) is presented. The model was built using precipitation data collected across eastern Oklahoma and northwestern Arkansas from late 2005 through early 2013. The dataset includes precipitation analyses at 4578 contiguous, 4 km x 4 km grid cells for 1800 precipitation events of 12 h. The dataset is unique in that the meteorological conditions for each 12-h event were relatively homogeneous when contrasted with single-point data obtained over months or years where the meteorological conditions for each rain event could have varied widely. Grid cells were counted and stratified by precipitation amount in increments of 0.05 in. (1.27 mm) up to 10 in. (254 mm), yielding histograms for each event. POEs were computed from the observed precipitation distributions and compared to POEs computed from two gamma probability density functions The errors between the observed POEs and gamma-computed POEs ranged between 2% and 10%, depending on the threshold POE selected for the comparison. This accuracy suggests the gamma models could be used to make reasonably accurate estimates of POE, given the percent areal coverage and the mean precipitation over the area. Finally, it is suggested that the areal distribution for each event is representative of the distribution at any point in the area over a large number of similar events. It then follows that the gamma models can be used to make forecasts for the probability of exceedance at a point, given the probability of rain and the expected mean rainfall at that same point.
机译:提出了一种优雅且易于实现的概率定量降水预测模型,该模型可用于估计超标概率(POE)。该模型使用2005年末至2013年初在俄克拉荷马州东部和阿肯色州西北部收集的降水量数据构建而成。该数据集包括4578个连续,4 km x 4 km网格单元中1800个12小时降水事件的降水量分析。该数据集的独特之处在于,与数月或数年获得的单点数据(每个降雨事件的气象条件可能变化很大)相比,每个12小时事件的气象条件相对均一。对网格单元进行计数,并以0.05英寸(1.27毫米)至10英寸(254毫米)为增量的降水量进行分层,从而生成每个事件的直方图。从观测到的降水分布中计算出POE,然后与从两个伽马概率密度函数计算出的POE进行比较。根据为比较选择的阈值POE,观测到的POE与伽马计算出的POE之间的误差在2%至10%之间。鉴于面积覆盖百分比和该地区的平均降水量,这种准确性表明伽马模型可用于对POE进行合理准确的估算。最后,建议每个事件的区域分布代表大量相似事件在区域中任何一点的分布。然后得出的结论是,给定下雨的概率和同一点的预期平均降雨量,伽马模型可用于预测某一点的超标概率。

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