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Seasonal rainfall forecasting for the Yangtze River basin using statistical and dynamical models

机译:使用统计和动态模型对长江流域的季节降雨预测

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摘要

Summer monsoon rainfall forecasting in the Yangtze River basin is highly valuable for water resource management and for the control of floods and droughts. However, improving the accuracy of seasonal forecasting remains a challenge. In this study, a statistical model and four dynamical global circulation models (GCMs) are applied to conduct seasonal rainfall forecasts for the Yangtze River basin. The statistical forecasts are achieved by establishing a linear regression relationship between the sea surface temperature (SST) and rainfall. The dynamical forecasts are achieved by downscaling the rainfall predicted by the four GCMs at the monthly and seasonal scales. Historical data of monthly SST and GCM hindcasts from 1982 to 2010 are used to make the forecast. The results show that the SST-based statistical model generally outperforms the GCM simulations, with higher forecasting accuracy that extends to longer lead times of up to 12 months. The SST statistical model achieves a correlation coefficient up to 0.75 and the lowest mean relative error of 6%. In contrast, the GCMs exhibit a sharply decreasing forecast accuracy with lead times longer than 1 month. Accordingly, the SST statistical model can provide reliable guidance for the seasonal rainfall forecasts in the Yangtze River basin, while the results of GCM simulations could serve as a reference for shorter lead times. Extensive scope exists for further improving the rainfall forecasting accuracy of GCM simulations.
机译:夏季季风降雨预测长江盆地对水资源管理和洪水和干旱控制非常有价值。然而,提高季节性预测的准确性仍然是一个挑战。在该研究中,应用统计模型和四种动态全球循环模型(GCMS)来对长江流域进行季节性降雨预测。通过建立海面温度(SST)和降雨之间的线性回归关系来实现统计预测。通过在每月和季节性尺度下抵制四个GCMS预测的降雨来实现动态预测。 1982年至2010年月度SST和GCM HindCasts的历史数据用于预测。结果表明,基于SST的统计模型通常优于GCM仿真,具有更高的预测精度,可延长到长达12个月的更长的延长时间。 SST统计模型达到高达0.75的相关系数,最低的平均相对误差为6%。相比之下,GCMS表现出急剧下降的预测精度,其超过1个月的交货时间。因此,SST统计模型可以为长江盆地的季节降雨预测提供可靠的指导,而GCM模拟的结果可以作为更短的交货时间的参考。存在广泛的范围,以进一步改善GCM模拟的降雨预测精度。

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