基于EMOS的多种集合预报后处理方法对比研究OA
Comparison of multiple ensemble forecast post-processing methods based on EMOS
数值天气预报的系统偏差通常需要后处理订正.EMOS(Ensemble Model Output Statistics)是一种针对集合预报的后处理方法,近年来逐渐发展出了两种衍生方法(gEMOS、SAMOS)来对它进行改进.因此,使用中国气象局的全球集合预报(GEPS)、全球确定性预报(GFS)、区域集合预报(REPS)以及两个不同空间分辨率的中尺度天气数值预报系统(MESO-10 km、MESO-3 km)共 5个数值模式,对华北地区 2 m气温、2 m相对湿度、10 m风速和 3 h累计降水量的预报订正效果进行了比较.结果表明,3种模式后处理方法均能有效提升对上述要素的预报效果,订正后的预报误差要小于所有输入的数值预报模式.(1)EMOS站点之间独立计算的方式能使得其保留站点的气候特征,因此在 3种方法中预报误差是最小的;(2)gEMOS由于忽略了站点的独立性,因此预报误差要高于 EMOS;(3)对 SAMOS而言,气温、湿度和风速这些气候态模拟较为准确的要素,预报误差能达到和 EMOS相同的水平,而对于降水这类偏态分布的变量,模拟的气候态影响了 SAMOS的订正效果,因此 SAMOS的预报误差要大于EMOS,但仍小于gEMOS.
Systematic biases in numerical weather prediction commonly require post-processing correction.Ensemble Model Output Statistics(EMOS)is a post-processing method for ensemble forecasts.In recent years,two other variations of EMOS(gEMOS and SAMOS)have been proposed to improve EMOS.This paper aims to evaluate their performance.A comparative study has been conducted for 2 m temperature,relative humidity,10 m wind speed,and 3 h cumulative precipitation in North China using five numerical models,i.e.,the Global Ensemble Prediction System(GEPS),the Global Forecast System(GFS),the Regional Ensemble Prediction System(REPS),and two mesoscale weather numerical forecasts(MESO-10 km,MESO-3 km)with different spatial resolutions from the China Meteorological Administration(CMA).Results show that all the three post-processing methods can reduce forecast errors of the CMA models across these variables.Specifically,(1)the EMOS method,which independently calculates parameters for each station,retains the unique characteristics of individual stations,resulting in optimal performance;(2)gEMOS underperforms EMOS due to its neglect of inter-station independence;(3)for variables such as temperature,humidity,and wind speed,which accurately simulate climatological distribution,SAMOS performance is comparable to that of EMOS.For precipitation,SAMOS's performance is constrained by climatological precipitation distribution simulation;the forecast error of SAMOS is larger than that of EMOS,yet it is still smaller than that of gEMOS.
霍自强;刘普;邓国;张玉涛;王勇;史屹翔
华风南信大研究院,南京,210044南京市气象局,南京,210019灾害天气科学与技术全国重点实验室,中国气象局地球系统数值预报中心,北京,100081灾害天气科学与技术全国重点实验室,中国气象局地球系统数值预报中心,北京,100081灾害天气科学与技术全国重点实验室,中国气象局地球系统数值预报中心,北京,100081||南京信息工程大学大气科学学院,南京,210044华风气象传媒集团,北京,100081
天文与地球科学
数值天气预报模式后处理集合预报EMOS
Numerical weather predictionPost-processingEnsemble forecastEMOS
《气象学报》 2026 (2)
262-275,14
国家自然科学基金(42475169)、中国气象局创新发展专项(CXFZ2025J011).
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