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    湘江流域TRMM卫星降水产品降尺度研究与应用

    Downscaling of TRMM precipitation products and its application in Xiangjiang River basin

    • 摘要: 为满足各行业对高分辨率、高精度降水数据的需求,以湘江流域为例,分别建立了基于多元线性回归法(multiple linear regression,MLR)和地理加权回归法(geographic weighted regression,GWR)的TRMM卫星降水降尺度模型,采用留一交叉验证法对模型进行优选,反演得到0.05°卫星-地面融合降水产品,并在此基础上分析了湘江流域的时空变化特征。结果表明: 相比热带降雨测量卫星(tropical rainfall measuring mission,TRMM)降水,降尺度后TRMM降水的空间分辨率得到大幅度提升,且与气象站点观测降水之间的决定系数平均提高了0.27以上,均方根误差和平均相对偏差平均降低了28.42 mm和29.88百分点以上,表明考虑植被、地形和地理要素的回归降尺度模型能够较为准确地刻画降水的空间分布特征; 相比MLR降尺度模型得到的降水,GWR降尺度模型得到的降水与气象站点观测降水之间的决定系数平均提高了0.06,均方根误差和平均相对偏差平均降低了14.88 mm和8.83百分点,表明GWR降尺度效果更好; 2006—2017年湘江流域不同时间尺度的降水时空变化特征迥异,表现在变化趋势及其显著性、对应区域的位置及面积上。

       

      Abstract: To meet the demand of various industries for high-resolution and high-precision precipitation data, this study establishes the downscaling models of the TRMM precipitation data of the Xiangjiang River basin based on the methods of multivariate linear regression (MLR) and geographically weighted regression (GWR). The leave-one-out cross-validation method was adopted to select the optimal model, and a satellite-ground fusion precipitation product with a resolution of 0.05° was obtained through inversion. On this basis, the spatial-temporal change characteristics of the precipitation in the Xiangjiang River basin were analyzed. The results are as follows. The spatial resolution of the TRMM precipitation data was greatly improved after downscaling. As verified using the precipitation observed at meteorological stations, the coefficient of determination of the TRMM precipitation data increased by more than 0.27, and the root mean square error and average relative error of the TRMM precipitation data decreased by more than 28.42 mm and 29.88 percentage points, respectively on average after downscaling. All these indicate that the regression downscaling model that takes account of vegetation, terrain, and geographic elements can accurately describe the spatial distribution characteristics of precipitation. According to the verification using the precipitation observed at meteorological stations, the coefficient of determination of the GWR downscaling model increased by 0.06 compared to the MLR downscaling model. Meanwhile, the root mean square error and average relative error of the precipitation data obtained using the GWR downscaling model decreased by 14.88 mm and 8.83 percentage points, respectively on average compared to precipitation data obtained using the MLR downscaling model. These indicate better effects of the GWR downscaling model. The spatial-temporal change characteristics of the precipitation in the Xiangjiang River basin during 2006—2017 are greatly different on different time scales, which is reflected in the changing trend and its significance and the locations and area of corresponding zones.

       

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