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ANALYSIS OF MULTIFRACTAL PROPERTIES OF TEMPORAL AND SPATIAL PRECIPITATION DATA IN JAPAN

机译:日本时空降水数据的多分形特性分析

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First, we examined scaling and multifractal properties of temporal precipitation data with an emphasis on the structure of the rainy vs. non-rainy periods, using the so-called β model. These data have scaling properties in a range of 1 day ≤ L_n ≤ 32 days. We characterize the scaling of the rainy areas with the single parameter of the β model and classified surface observation stations into two groups according to the parameter; namely, along the Pacific Ocean and Japan Sea coasts. The Pacific Ocean data are more intermittent and peaky than the Japan Sea data and exhibit more multifractality than the latter. Second, we analyzed the time variation of scaling properties of several months of spatial radar data using the intercept of the regression estimate of the scaling of the fractional wetted area. These results showed that over the sea in the summer, there was a tendency for a different scaling of small vs. large scales. Finally, we extracted four independent precipitation events from the whole dataset and examined whether or not a one-to-one function can represent the relationship between mesoscale forcing and the parameter of the β model. We conclude that there is a one-to-one functional relationship if we consider each precipitation event separately and exclude multiple independent precipitation events.
机译:首先,我们使用所谓的β模型研究了时间降水数据的标度和多重分形特性,重点是雨季与非雨季的结构。这些数据具有在1天≤L_n≤32天的范围内的缩放属性。我们用β模型的单个参数来表征雨区的尺度,并根据该参数将地表观测站分为两组。即沿太平洋和日本海沿岸。太平洋的数据比日本海的数据更断断续续,且峰值更大,并且比日本海数据显示出更多的多重分形性。其次,我们使用分数润湿区域的比例回归估计值的截距分析了几个月空间雷达数据的比例特性的时间变化。这些结果表明,夏季在海上,小尺度和大尺度存在不同的缩放趋势。最后,我们从整个数据集中提取了四个独立的降水事件,并检查了一对一函数是否可以表示中尺度强迫与β模型参数之间的关系。我们得出的结论是,如果我们分别考虑每个降水事件并排除多个独立的降水事件,则存在一对一的函数关系。

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