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Representing the precipitation regime by means of Fourier series

机译:用傅里叶级数表示降水状态

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We propose the use of Fourier series for representing the precipitation regime in a certain location and predicting it in ungauged locations, allowing for map production. We analyse monthly average precipitation data of 2043 gauging stations covering the Italian territory. The Fourier series allows to represent a curve as a sum of different sinusoidal components characterized by their period, amplitude and phase. Being the different harmonics not correlated, it is possible to fit them with stepwise multiple linear regressions. The Fourier series allows for a parsimonious representation of the regime, being usually the 12- and 6-month harmonics able to reproduce the observed values with little residuals [in this exercise the fitting gave an average monthly root mean square error (RMSE) of 9.21 mm and a correlation coefficient of 0.979]. Once the at-station harmonics parameters are obtained, it is possible to map them for predicting the regime in ungauged locations. Here we use ordinary kriging and the leave-one-out validation scheme for evaluating the amplitudes and phases of the harmonics of the 12- and 6-month periods and reconstructing the precipitation regime. We use the same scheme for the interpolation of the station data on a month-by-month basis, whose results are used as a benchmark. The analyses provide similar results, with overall RMSEs of 17.53 and 15.97 mm and correlation coefficients of 0.909 and 0.921, respectively. The spatial patterns of the reconstruction error are similar for the two cases. The stations having higher RMSE are clustered in the areas presenting high precipitation gradients, such as in the Appennines, or where major precipitation regime changes occur. For demonstrating that the Fourier series approach is more suitable for regionalization purposes, a k-means cluster analysis on the Fourier parameters was performed and the effect of such stratification on the mapping of the precipitation regime by applying regression kriging was assessed.
机译:我们建议使用傅里叶级数来表示某个位置的降水状况,并在未定位的位置进行预测,从而生成地图。我们分析了覆盖意大利领土的2043个测量站的月平均降水量数据。傅里叶级数允许将曲线表示为不同正弦波分量的总和,这些正弦波分量的周期,幅度和相位为特征。由于不同的谐波不相关,因此可以通过逐步多元线性回归拟合它们。傅里叶级数可以简化表示该状态,通常是12个月和6个月的谐波能够再现几乎没有残差的观测值[在本练习中,拟合给出的平均月均方根误差(RMSE)为9.21毫米和相关系数0.979]。一旦获得了站内谐波参数,就可以将其映射以预测未开启位置的状态。在这里,我们使用普通克里金法和留一法验证方案来评估12个月和6个月期间谐波的振幅和相位,并重建降水状态。我们按月对插值数据使用相同的方案,其结果被用作基准。这些分析提供了相似的结果,总体RMSE为17.53和15.97 mm,相关系数分别为0.999和0.921。两种情况下重建误差的空间模式相似。具有较高RMSE的台站聚集在降水梯度高的区域,例如在Appennines或发生主要降水变化的地区。为了证明傅里叶级数方法更适合于区域化目的,对傅里叶参数进行了k均值聚类分析,并通过应用回归克里金法评估了这种分层对降水状况制图的影响。

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