华东地区一次中尺度对流云系过程与气溶胶相互作用的数值模拟
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P426

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中国气象局中部区域人工影响天气能力建设项目(ZQC-T22253) ;国家自然科学基金资助项目(42275078);国家重大科技基础设施项目


Numerical simulation of the cloud-aerosol interactions in mesoscale convective cloud processes over eastern China
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    摘要:

    本文利用耦合了化学模式的中尺度气象数值模式WRF-Chem,对2019年华东地区一次中尺度对流天气过程进行模拟,着重研究了人为活动生成的气溶胶对于云降水宏微观结构和演变过程的影响以及云降水过程对气溶胶的湿清除作用。研究发现,由于人为排放源的加入,研究期间内的地表降水减弱,云中凝结和凝华过程受到抑制,云内对流核心区的垂直气流速度整体减弱,最终抑制了对流的发展。云中除云滴外,雨滴、冰晶、雪和霰的质量浓度均在12 km以下减少。对于雨、雪和霰的质量浓度源汇项分析发现,雨水含量的减少主要是由于雨滴碰并云滴和霰的融化受到抑制,导致雪和霰减少的主要微物理过程均与0 ℃层以上的过冷水含量有关。上述微物理过程减弱的峰值高度与水成物粒子质量浓度减少的峰值高度均有较好的对应。云中微物理过程的增强或减弱同样作用于云中活化气溶胶清除过程,对于模拟期间云滴(活化气溶胶)清除特征的研究发现,在污染情况下,云滴的清除量增多,但清除率降低。清除率的差异主要归因于雨滴对云滴的碰并过程。而污染情况下的清除量增多则是由于其云滴数浓度本身较大,即使清除率较低,也能清除较多的云滴。污染情况下雨滴的质量浓度和数浓度均减少,但碰并消耗的云滴数量增多。

    Abstract:

    A mesoscale convective system occurred over eastern China in 2019 was simulated using the Weather Research and Forecasting model coupled with chemistry (WRF-Chem) in order to investigate the effects of aerosols from anthropogenic emission on the macro-and microstructure and evolution of cloud system, as well as the wet scavenging effect of cloud and precipitation processes on aerosols. Results show that surface precipitation weakened during the study period due to enhanced pollutants, and condensation and deposition suppressed, resulting in reduced vertical velocity in the convective core area, which ultimately suppresses the development of convection. The mass concentrations of raindrops, ice crystals, snow, and graupel below 12 km of altitude all decreased except for cloud droplets. The analysis of the source-sink terms for the mass concentrations of rain, snow, and graupel reveals that the decrease in rainwater content is mainly due to the inhibition of the melting of graupel and collection of cloud droplets by raindrops. The dominant microphysical processes leading to the decrease in snow and graupel mixing ratio are related to the supercooled water content. The peak heights of the weakening of these microphysical processes corresponded well to the ones of the reduction in the mass concentration of hydrometeors. The enhancement or inhibition of cloud microphysical processes acts on the removal of activated aerosol. The analysis of removal characteristics of cloud droplet (activated aerosol) during the study period reveals that the number of scavenged cloud droplet increases, but the scavenging rate decreases in the polluted case. The difference in the scavenging rate is mainly attributed to the collection of cloud droplets by raindrops. The increasing removal amount in the polluted case is due to its larger cloud droplet number concentration, which removes more cloud droplets even though the scavenging rate is lower. The mass and number concentration of raindrops decreased, but the number of cloud droplets consumed by collection process increased in the pollution case.

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张子涵,陈倩,周学东,郭俊,王佳,况祥,吴奕霄.华东地区一次中尺度对流云系过程与气溶胶相互作用的数值模拟.气象科学,2025,45(5):690-703 ZHANG Zihan, CHEN Qian, ZHOU Xuedong, GUO Jun, WANG Jia, KUANG Xiang, WU Yixiao. Numerical simulation of the cloud-aerosol interactions in mesoscale convective cloud processes over eastern China. Journal of the Meteorological Sciences,2025,45(5):690-703

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  • 收稿日期:2024-05-02
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  • 在线发布日期: 2026-03-06
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