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The use of personal weather station observations to improve precipitation estimation and interpolation

机译:使用个人气象站观察来提高降水估算和插值

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The number of personal weather stations?(PWSs) with data available through the internet is increasing gradually in many parts of the world. The purpose of this study is to investigate the applicability of these data for the spatial interpolation of precipitation using a novel approach based on indicator correlations and rank statistics. Due to unknown errors and biases of the observations, rainfall amounts from the PWS network are not considered directly. Instead, it is assumed that the temporal order of the ranking of these data is correct. The crucial step is to find the stations which fulfil this condition. This is done in two steps – first, by selecting the locations using the time series of indicators of high precipitation amounts. Then, the remaining stations are then checked for whether they fit into the spatial pattern of the other stations. Thus, it is assumed that the quantiles of the empirical distribution functions are accurate. These quantiles are then transformed to precipitation amounts by a quantile mapping using the distribution functions which were interpolated from the information from the German National Weather Service?(Deutscher Wetterdienst – DWD) data only. The suggested procedure was tested for the state of Baden-Württemberg in Germany. A detailed cross validation of the interpolation was carried out for aggregated precipitation amount of?1, 3, 6, 12?and 24?h. For each of these temporal aggregations, nearly 200?intense events were evaluated, and the improvement of the interpolation was quantified. The results show that the filtering of observations from PWSs is necessary as the interpolation error after the filtering and data transformation decreases significantly. The biggest improvement is achieved for the shortest temporal aggregations.
机译:个人气象站的数量?(PWSS)通过互联网提供的数据在世界许多地方逐渐增加。本研究的目的是使用基于指标相关性和等级统计数据的新方法来研究这些数据的适用性降水的空间插值。由于观察结果的未知错误和偏见,PWS网络的降雨量不直接考虑。相反,假设这些数据的排名的时间顺序是正确的。关键步骤是找到满足这种情况的站。这是以两步完成的 - 首先,通过使用高降水量的时间序列选择位置来选择位置。然后,然后检查其余站是否适合其他站的空间图案。因此,假设经验分布函数的量级是准确的。然后使用使用从德国国家天气服务的信息中插值的分配函数将这些量级转换为降水量?(Deutscher Wetterdienst - DWD)数据。建议的程序为德国巴登 - 符腾堡州的州进行了测试。对插值的详细交叉验证用于聚集的沉淀量的α1,3,6,12?和24μm。对于这些时间聚集中的每一个,评估了近200的发生事件,量化了插值的改善。结果表明,在过滤和数据变换显着降低后,将从PWSS的观测过滤是必要的。最短的时间聚合实现了最大的改进。

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