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CMA-MESO模式对华东地区夏季降水预报偏差分析

Assessing Biases in CMA-MESO Summer Precipitation Forecasts over East China

  • 摘要: CMA-MESO模式(China Meteorological Administration Mesoscale Model)是降水预报业务重要支撑,但每天8次滚动更新预报使得预报评估面临新挑战,理解平均偏差特征、不同预报时效特征差异以及误差来源,是改进模式的关键。本文系统分析了2023年夏季华东地区CMA-MESO模式降水预报性能,结果表明:(1)多时效预报平均能较好地再现观测降水空间分布特征,但在降水量级和发生频率方面存在系统性偏差。(2)模式对中雨及以上量级的降水量预报存在明显高估,对无降水事件频率预报较观测偏低3.7%,对小雨事件频率预报偏高2.6%,且对大雨及以上量级降水事件的空报率较高。(3)预报性能呈现显著的时效依赖性,降水偏差在3~6 h短临预报时达到最大值,随后随预报时效增加逐渐减小,在21~24 h达到最小值,并在24~36 h阶段再次增大。(4)物理原因分析表明,短临预报的降水高估与云分析同化引入过多水物质有关,而24 h后预报偏强则源于模式低层风速预报偏强导致的水汽输送过量。

     

    Abstract: The China Meteorological Administration Mesoscale Model (CMA-MESO) serves as a critical operational system for precipitation forecasting. However, its eight-times-daily rolling updates present new challenges for forecast evaluation. A comprehensive understanding of mean bias characteristics, variations across different forecast lead times, and error sources is key to model improvement. This study systematically evaluated the precipitation forecast performance of the CMA-MESO over East China during the summer of 2023. The key findings are as follows: (1) While the averaged multiple forecasts generally reproduced the spatial distribution patterns of observed precipitation, systematic biases existed in precipitation intensity and frequency. (2) The model significantly overestimated the precipitation amount for moderate-and-above rainfall events, with 3.7% underestimation of the frequency of no-rainfall events but 2.6% overestimation of the frequency of light rain events, along with elevated false alarm rates for heavy-and-above rainfall events. (3) The forecast performance showed a distinct lead-time dependence, with precipitation biases largest in 3~6 h nowcasting, gradually decreasing to a minimum in 21~24 h forecasts, and then increasing again in the 24~36 h range. (4) Physical analysis revealed that the nowcasting overestimation stemmed from excessive hydrometeor introduction during cloud analysis, and the overestimation in the forecast after 24 h resulted from excessive low-level wind speeds that promoted moisture transport to the target region.

     

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