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作 者:李超 陈潜 赵春阳 张超 LI Chao;CHEN Qian;ZHAO Chunyang;ZHANG Chao(Meteorological Bureau of Shenzhen Municipality,Shenzhen 518040,China;Shenzhen National Climate Observatory,Shenzhen 518040,China;Shenzhen Key Laboratory of Severe Weather in South China,Shenzhen 518001,China)
机构地区:[1]深圳市气象局,广东深圳518040 [2]深圳国家气候观象台,广东深圳518040 [3]深圳市南方强天气研究重点实验室,广东深圳518001
出 处:《海洋气象学报》2021年第2期24-33,共10页Journal of Marine Meteorology
基 金:国家重点研发计划“政府间国际科技创新合作/港澳台科技创新合作”重点专项项目(2019YFE0110100);国家自然科学基金项目(41405047,41975124);深圳市基础研究专项重点项目(JCYJ20200109113014456);浙江省自然科学基金项目(LY20D050001)。
摘 要:在高空槽和低层切变线配合的相似环流背景下,2019年4月11日深圳出现短时暴雨(简称“2019年过程”),2020年4月11日以稳定性弱降水为主(简称“2020年过程”),利用ERA5再分析数据等对深圳这两次前汛期降水过程进行了对比分析。结果表明,2019年过程,温湿层结等对流条件和高空辐散条件较好,低空辐合动力条件相对较弱,在边界层辐合线触发下产生明显的中尺度对流系统(mesoscale convective system,MCS)活动,导致深圳出现短时强降水和雷暴大风。2020年过程,低层辐合等动力条件较好,但对流条件相对较弱,降水以稳定性降水为主。对比分析说明,温度和湿度层结条件较动力条件对华南前汛期MCS生成作用更为明显,强对流发生前12 h深圳等珠三角地区Q矢量辐合明显,对MCS活动以及强对流发生有较好的指示意义。In Shenzhen,a short-lived rainstorm accompanied by gale occurred on 11 April 2019,while a weak stable precipitation event happened on 11 April 2020.The two distinct rainfall events take place in the similar circulation backgrounds of upper-level trough and lower-level shear.The features and associated mechanisms of the two events in the early rainy season are analyzed by using ERA5 reanalysis data.The short-lived rainstorm in 2019 comes along with a typical mesoscale convective system(MCS),which migrates eastwards and leads to the short-time torrential rain and thunderstorm gale in Shenzhen.The MCS is triggered by the boundary layer convergence line,and then develops in good convective conditions of temperature and humidity and divergence at upper level,but unfavorable dynamic conditions such as weak convergence at lower level.In contrast,Shenzhen sees a much more tender and stable rain in 2020,which happens in the beneficial dynamic conditions of lower-level convergence but weak convective conditions.The comparison suggests the convective conditions such as temperature and humidity play more important role than dynamic conditions in the development of MCSs in the early rainy season of South China.The Q-vector shows significant convergence over Pearl River Delta areas such as Shenzhen up to 12 h in advance of the strong convection,which is a skillful precursor for the occurrence of MCS and convection.
分 类 号:P458.3[天文地球—大气科学及气象学]
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