摘要
利用自动站小时降水资料、常规观测资料、欧洲中心细网格和GRAPES-GFS数值模式产品、NCEP和ERA5再分析资料,对2021年5月10日~12日邵阳市暴雨、冰雹天气过程进行分析。结果表明:此次暴雨是在高空槽东移、低空急流、低空切变线共同作用下发生的。白天地面倒槽的发展、地面辐合线对暖区暴雨、冰雹、雷暴大风等天气有一定的指示作用。临近的中尺度模式对于暴雨、大暴雨有指示意义。
The rainstorm and hail weather process in Shaoyang from 10~12 May, 2021 is analyzed by using the hourly precipitation data of automatic stations, conventional observations, the European Center fine grid and the GRAPES-GFS numerical model products, NCEP and ERA5 reanalysis data. The results show that the rainstorm occurred under the joint action of the eastward movement of the high trough, the low-level jet stream and the low-level shear line. The development of surface troughs during the day and the convergence line of the ground have a certain indicative effect on weather conditions such as heavy rain, hail, thunderstorms, and strong winds in warm regions. The adjacent mesoscale model is indicative of rainstorm and heavy rainstorm.
出处
《气候变化研究快报》
2023年第5期979-988,共10页
Climate Change Research Letters