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1961–1990 high-resolution Northern and Central Italy monthly precipitation climatologies

机译:1961–1990年意大利北部和中部高分辨率的每月降水气候

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Monthly Northern and Central Italy precipitationclimatologies, obtained by means of a procedure aiming at capturing thelocal dependence of precipitation on elevation, are presented. The procedureconsists in considering each cell of a high-resolution grid and in makinguse of the closest 15 stations in order to perform a weighted linearregression of precipitation versus elevation: the weights are determined bythe distances of the stations from the grid point and by the level ofsimilarity between the stations' cells and the considered grid cell in termsof elevation, slope steepness, slope orientation and distance from the sea.The study is based on a dataset of about 3200 1961–1990 monthly precipitationnormals. The performance of the procedure is evaluated by reconstructing themonthly precipitation normals of each station and by comparing them with thecorresponding observed values. Such comparisons are performed by means offive error estimators: the mean absolute error and the mean error, bothevaluated in absolute and relative form, and the root mean squared error.The mean absolute error is slightly more than 10 mm for the monthlyprecipitation, which turns out to be between 10% and 14% of themonthly precipitation.
机译:介绍了意大利北部和中部的每月降水气候,这些气候是通过一种旨在捕获降水对海拔高度的局部依赖性的程序而获得的。该程序包括考虑高分辨率网格的每个像元以及利用最接近的15个站点以进行降水量与海拔高度的加权线性回归:权重由站点距网格点的距离和相似程度确定在海拔,坡度,坡度方向和距海的距离方面,这些站点位于观测站的网格与考虑的网格单元之间。该研究基于约3200个1961–1990月降水法线的数据集。通过重建每个气象站的每月降水正常值并将其与相应的观测值进行比较,可以评估该过程的性能。这种比较是通过均值误差估计器进行的:均值绝对误差和均值误差(均以绝对和相对形式进行评估)以及均方根均方根误差。月降水量的均值绝对误差略大于10 mm,结果在月降水量的10%到14%之间。

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