基于滑动质心法的华南地区锋面和暖区降水ECMWF模式预报性能评估OACSTPCD
Evaluation of ECMWF model forecasting performance for front and warm-area rainfall in South China based on the sliding centroid method
应用空间滑动质心法对2018-2020 年华南地区锋面和暖区中雨、大雨及暴雨量级降水ECMWF模式(简称EC模式)24~168 h时效的空间落区预报结果进行定量分析.结果表明:EC模式对华南暖区降水和锋面暴雨的空间落区预报存在系统性经纬向偏差,且以偏西北为主;对锋面中雨和大雨的空间落区预报存在系统性经向偏差,且以偏北为主,但纬向偏差不明显.模式对锋面和暖区降水空间落区预报的纬度偏差分别集中在1.0°和1.5°以内,经度偏差分别集中在1.5°和2.0°以内.随预报时效增加,EC模式的空间预报偏差增大,24~72 h时效的EC模式空间落区预报相对稳定,96~168 h时效的预报偏差明显增大.2022 年华南地区两次锋面和暖区降水空间位置质心订正结果表明,订正后的模式降水TS评分明显提高.
Based on the sliding centroid method,the spatial rainfall location forecast performance of EC model in 24~168 h for moderate,heavy,and torrential rainfall in the front and warm areas of South China was analyzed.The results show that the ECMWF model(abbreviated as EC model)has systematical meridional and zonal devia-tion in warm-area rainfall and front rainstorm location,and the forecasted rainfall location is located west and north to the observed one.The location deviation of front moderate rain and heavy rain is dominantly meridional ones,in which cases with north rainfall deviation are more than the south one.The zonal displacement error is not clear.The meridional deviation of front and warm-area rainfall location lies in 1.0°and 1.5°,respectively.The zonal de-viation lies in 1.5°and 2.0°,respectively.The spatial rainfall location forecast performance of EC model is differ-ent with the different valid time,which is relatively stable in 24~72 h.The forecast deviation in 96~168 h increa-ses obviously.A method for correcting the spatial rainfall location is established.The deviation correction method is applied to two rainfall events in 2022,and the results show that the TS scores can be significantly improved.
魏蕾;陈炳洪;张兰;李怀宇;梁之彦;许欢
广州市气象台,广东广州 511430
大气科学
滑动质心法预报时效空间偏差
Sliding centroid methodForecast lead timeSpatial deviation
《气象与环境学报》 2024 (002)
9-16 / 8
中国气象局创新发展专项(CXFZ2022J006)、广州市科技计划项目(202103000030)、广东省气象局智能网格预报技术创新团队项目和国家自然科学基金项目(U2142213)共同资助.
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