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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >A hybrid statistical downscaling model for prediction of winter precipitation in China
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A hybrid statistical downscaling model for prediction of winter precipitation in China

机译:预测中国冬季降水的混合统计降尺度模型

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Downscaling techniques can effectively improve the coarse resolution and poor representation of precipitation predicted by general circulation model (GCM). In this study, a statistical downscaling (SD) method, based on the singular value decomposition (SVD), is proposed for better representing the coupled variation between predictors and winter precipitation in China. By comparing current predictors from Climate Forecast System version 2 (CFSv2) of National Centers for Environmental Prediction and previous predictors from observation, the two best appropriate predictors, the winter sea level pressure (SLP) from the CFSv2 and the autumn sea-ice concentration (SIC) from observation, are selected to construct the SD model for prediction of winter precipitation in China. Three downscaling schemes are developed by involving the SLP, SIC, and both of them (i.e. SLP-scheme, SIC-scheme, and SS-scheme), respectively. Validations for the schemes show a considerable improvement of performance in predicting China winter precipitation, compared with the original CFSv2 output. The temporal and spatial anomaly correlation coefficient (ACC) and root mean square errors (RMSE) were estimated. For the cross validation, the spatial ACC are increased from approximate to 0.01 of the CFSv2 to >0.3 of the downscaling model. For the independent validation, the temporal RMSE from the downscaling schemes are all decreased more than 30%. In particular, the results using the SS-scheme showed relatively smaller RMSE than those of either the SLP-scheme or SIC-scheme, and hence can reproduce the precipitation anomaly in 2011 and 2012 winters more accurately.
机译:降尺度技术可以有效地改善一般循环模型(GCM)预测的降水的粗分辨率和不良表示。在这项研究中,提出了一种基于奇异值分解(SVD)的统计降尺度(SD)方法,以更好地表示中国的预报因子与冬季降水之间的耦合变化。通过比较国家环境预测中心的气候预测系统第2版(CFSv2)的当前预测因子和先前的观测预测因子,可以比较两种最合适的预测因子:CFSv2的冬季海平面压力(SLP)和秋季海冰浓度(从观测中选择SIC,以构建SD模型来预测中国的冬季降水。通过涉及SLP,SIC以及它们两者(分别是SLP方案,SIC方案和SS方案),开发了三种缩减方案。与原始CFSv2的输出相比,该方案的验证表明,在预测中国冬季降水方面的性能有了很大提高。估计了时空异常相关系数(ACC)和均方根误差(RMSE)。对于交叉验证,空间ACC从CFSv2的大约0.01增加到缩小模型的> 0.3。对于独立验证,按比例缩小方案的时间RMSE均降低了30%以上。特别是,使用SS方案的结果显示RMSE相对小于SLP方案或SIC方案的RMSE,因此可以更准确地再现2011年和2012年冬季的降水异常。

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