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气象:2025,51(4):473-483
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惠州前汛期暖区暴雨环流分型及其环境参量统计分析
付智龙,姜帅,李国平,陈芳丽,黄楚贤,骆蓉,张秋明,梁惠龙
(广东省惠州市惠阳区气象局,惠州 516211; 广东省惠州市气象局,惠州 516001; 广东省惠州市突发事件预警信息发布中心,惠州 516001; 成都信息工程大学大气科学学院,成都 610225)
Statistical Analysis on Classification of Synoptic Circulation of Warm-Sector Heavy Rainfall and Its Ambient Parameters in Huizhou During the First Rainy Season
FU Zhilong,JIANG Shuai,LI Guoping,CHEN Fangli,HUANG Chuxian,LUO Rong,ZHANG Qiuming,LIANG Huilong
(Huiyang Meteorological Station of Huizhou City of Guangdong Province, Huizhou 516211; Huizhou Meteorological Office of Guangdong Province, Huizhou 516001; Huizhou Emergency Warning Information Dissemination Center of Guangdong Province, Huizhou 516001; School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225)
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投稿时间:2024-02-03    修订日期:2025-02-06
中文摘要: 利用自动气象站雨量资料、ERA5再分析数据对2003—2022年4—6月惠州前汛期暖区暴雨个例进行挑选和环流分型,对比分析了不同类型暖区暴雨发生时的平均环流场和环境场特征。得到以下主要结果:2003—2022年惠州前汛期共发生48次暖区暴雨,可以分为切变型(第一类)、短波槽+低空急流型(第二类)和副热带高压外围+低空急流入口型(第三类)。进一步对比各类暖区暴雨的平均环流场发现,在500 hPa上除第二类暴雨受到短波槽影响外,其余两类暴雨惠州地区都处于西风气流、副热带高压外围西南气流的控制之下;在低层,第二、三类暴雨惠州附近都出现了双低空急流(西南低空急流和边界层低空急流),而第一类暴雨只在925 hPa珠江口以南出现了边界层低空急流。环境场特征分析表明,ERA5再分析资料计算的环境参量具有一定的可信度和适用性,第二、三类暴雨整体上水汽和能量条件优于第一类暴雨,但对于动力条件而言,第一类暴雨的垂直风切变则明显高于第二、三类暴雨,同时第一类暴雨的静力不稳定度也要高于其余两类暴雨。
Abstract:Based on the precipitation data from automatic weather stations and ERA5 reanalysis data, case seletion and classification of synoptic circulation are carried out in this paper to study the warm-sector heavy rainfall in Huizhou during the first rainy season from April to June of 2003-2022. And a comparative analysis is conducted on characteristics of average synoptic circulation and ambient parameters between different types of warm-sector rainfall events. The results show that a total of 48 warm-sector heavy rainfall events occurred in Huizhou during the first rainy season in 2003-2022. Accroding to synoptic circulation, the selected warm-sector rainfall events are divided into three types, i.e., shear line (the first type), shortwave trough with low-level jet (the second type), and the edge of subtropical high with the entrance of low-level jet (the third type). By further comparing the average synoptic circulation between different types of warm-sector rainfall events, we reveal that Huizhou is under the control of the west wind flow and the southwest flow in the periphery of subtropical high at 500 hPa, except the second type of heavy rainfall. In low levels, there are double low-level jet (southwest low-level jet and boundary layer low-level jet) near Huizhou both in the second and third types of heavy rainfall, while in the first type of heavy rain, there is boundary layer low-level jet only to the south of the Pearl River Estuary at 925 hPa. The analysis of the ambient features indicates that the ambient parameters calculated based on ERA5 reanalysis are reliable and applicable. The second and third types of heavy rainfall are superior to the first type of heavy rainfall in moisture and energy conditions. But in terms of dynamic conditions, the vertical wind shear, and the static instability of the first type of heavy rainfall is considerably stronger than those of the other two types of heavy rainfall.
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基金项目:国家自然科学基金项目(42175002、42075013)和广东省气象局科学技术研究项目(GRMC2021M23、GRMC2022M29、GRMC2024Q27)共同资助
引用文本:
付智龙,姜帅,李国平,陈芳丽,黄楚贤,骆蓉,张秋明,梁惠龙,2025.惠州前汛期暖区暴雨环流分型及其环境参量统计分析[J].气象,51(4):473-483.
FU Zhilong,JIANG Shuai,LI Guoping,CHEN Fangli,HUANG Chuxian,LUO Rong,ZHANG Qiuming,LIANG Huilong,2025.Statistical Analysis on Classification of Synoptic Circulation of Warm-Sector Heavy Rainfall and Its Ambient Parameters in Huizhou During the First Rainy Season[J].Meteor Mon,51(4):473-483.