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摘要
为提高降水集合预测精度和可靠性,需对数值模式预测降水进行误差订正。以汉江上游流域为研究区域,构建机器学习降水预测误差订正方法即分位数回归森林(quantile regression forest,QRF),对欧洲中期天气预报中心(European Centre for Medium-Range Weather Forecasts, ECMWF)模式次季节尺度逐日降水预测结果进行误差订正,并与传统降水预测误差订正方法中的分位数映射(quantile mapping,QM)、贝叶斯联合概率(Bayesian joint probability,BJP)进行对比。从集合预报角度,分析不同误差订正方法精度和可靠性差异。结果表明:与 ECMWF 模式预测结果相比,QM、BJP、QRF 方法均可以有效提高原始降水集合预测精度,BJP 方法订正后预测精度略高于 QRF 方法,QM 方法最低;不同误差订正方法预测降水精度均随着预见期的延长而降低,当预见期达到 20 d 以上时,BJP 和 QRF 方法预测精度和气候预测相当;QM 方法和 ECMWF 模式预测结果低于气候预测精度;ECMWF 模式预测和 QM 方法订正后预测降水的可靠性均较低。BJP 和 QRF 方法均能够提高降水集合预测的可靠性,且 QRF 方法的可靠性高于 BJP 方法。研究成果可为汉江上游流域水旱灾害防御、水资源优化配置提供重要支撑。
Abstract
Water resource managers and users received crucial information from skillful sub-seasonal precipitation forecasts (between two weeks and three months). Sub-seasonal forecasts remained difficult because predictability from initial atmospheric conditions faded after two weeks and variability in the lower boundary was too short to be effective at this time scale. With a better understanding of potential predictability sources and the development of dynamical climate models, sub-seasonal forecasts have advanced dramatically. In recent years, many operational centers have developed Global Climate Models (GCMs) to provide routine subseasonal precipitation forecasts. Nevertheless, the GCM precipitation forecasts were always biased, as discrepancies existed between the numerical approximations of the Earth's system and the real world. Furthermore, the ensemble spread of GCMs was frequently insufficient to provide accurate forecasts. It was necessary to correct GCM precipitation forecasts to improve their accuracy and reliability before they could be used for hydrological applications such as flood and drought disaster prevention and water resource management. Over the last two decades, several traditional statistical error correction methods have been proposed to improve forecast accuracy and reliability, including Bayesian joint probability, censored and shifted gamma distribution, quantile mapping (QM), and others. However, statistical error correction methods were based on probabilistic distribution assumptions, which proved problematic for skewed precipitation data. Machine learning methods could capture the nonlinear relationships among variables and were gradually applied in the field of error correction for precipitation forecasts in recent years, including random forest and eXtreme gradient boosting. The machine learning methods did not rely on the statistical assumptions and were of great potential application. However, because uncertainty was not taken into account, the majority of machine learning techniques were unable to produce probabilistic forecasts. The quantile regression forests (QRF), a variant of random forests (RF), could not only predict the conditional mean, but also generate the complete conditional probability distribution. Studies proved that the QRF method could improve wind and temperature forecast skill. However, the application of QRF on correcting precipitation forecasts was less. Meanwhile, the impact of various error correction methods on sub-seasonal precipitation ensemble forecasts remained to be investigated. QRF method was applied to correct the daily precipitation forecast results of the ECMWF (European Centre for Medium-Range Weather Forecasts) model at the sub-seasonal scale over the Upper Hanjiang River basin. The forecast accuracy and reliability were assessed through a leave-one-year-out cross-validation using continuous ranked probability skill score andα-index. We further compared the performance of the QRF method with that of two traditional error correction methods for precipitation forecasts, including QM and BJP. The QM, BJP, and QRF methods all significantly improved the accuracy of the original ensemble precipitation forecasts when compared to those derived directly from the ECMWF model. However, these methods differed in some respects. The BJP method yielded slightly higher forecast accuracy after correction than the QRF method, and the QM method performed the poorest. The precipitation forecast accuracy of all error correction methods decreased with the extension of lead time. When the lead time exceeded 20 days, the forecast accuracy of the BJP and QRF methods was comparable to that of climatic forecasts, while the forecast accuracy of the QM method and the original ECMWF model was lower than that of climatic forecasts. Both the precipitation forecasts of the ECMWF model and those corrected by the QM method showed low reliability. In contrast, the BJP and QRF methods could both improve the reliability of ensemble precipitation forecasts, with the QRF method outperforming the BJP method in terms of reliability. These findings provided important support for flood and drought disaster prevention and optimal allocation of water resources in the Upper Hanjiang River basin.
关键词
Key words
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田晴,李源.
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南水北调与水利科技(中英文), 2026, 24(4): 878-888 DOI:10.13476/j.cnki.nsbdqk.2026.0082
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基金资助
国家自然科学基金面上项目(52579004)