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This paper proposes a simple and powerful optimal integration (OPI) method for improving hourly quantitative precipitation forecasts (QPFs, 0-24 h) of a single-model by integrating the benefits of different bias- corrected methods using the high-resolution CMA-GD model from the Guangzhou Institute of Tropical and Marine Meteorology of China Meteorological Administration (CMA). Three techniques are used to generate multi-method calibrated members for OPI: deep neural network (DNN), frequency-matching (FM), and optimal threat score (OTS). The results are as follows: (1) The QPF using DNN follows the basic physical patterns of CMA-GD. Despite providing superior improvements for clear-rainy and weak precipitation, DNN cannot improve the predictions for severe precipitation, while OTS can significantly strengthen these predictions. As a result, DNN and OTS are the optimal members to be incorporated into OPI. (2) Our new approach achieves state-of-the-art performances on a single model for all magnitudes of precipitation. Compared with the CMA-GD, OPI improves the TS by 2.5%, 5.4%, 7.8%, 8.3%, and 6.1% for QPFs from clear-rainy to rainstorms in the verification dataset. Moreover, OPI shows good stability in the test dataset. (3) It is also noted that the rainstorm pattern of OPI relies heavily on the original model and that OPI cannot correct for deviations in the location of severe precipitation. Therefore, improvements in predicting severe precipitation using this method should be further realized by improving the numerical model’s forecasting capability. 相似文献
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应用常规资料、TBB资料和NCEP分析资料,对2007年7月25日发生在湘黔边境的一次梅雨锋大暴雨天气过程进行了分析.结果表明:深厚的高空低槽和副热带高压稳定维持,有利于冷暖空气的辐合和梅雨锋的长时间维持.梅雨锋上不断有中小尺度对流系统产生,这些中小尺度对流系统在受到大尺度强迫作用和梅雨锋自身的强迫抬升作用而发展增强并长时间维持,在暴雨区形成强烈的降水.暴雨区上空具有低层辐合、高层辐散的结构特征,低层的辐合使得涡度往中上层输送,这种耦合形势有利于垂直上升运动和暴雨的维持.积云对流释放的凝结潜热加热对流层中上层大气,引起梅雨锋锋生,维持和促进了垂直上升运动和对流活动. 相似文献
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