作者:吴亚丽,高郁东,陈德辉,蒙伟光,林良勋,林文实
摘要:Warm-sector torrential rainfall(WSTR)events that occur in the annually first rainy season in south China are characterized by high rainfall intensity and low radar echo centroids.To understand the synoptic characteristics related to these features,16 WSTR events that occurred in 2013-2017 were examined with another 16 squall line(SL)events occurred during the same period as references.Composite analysis derived from ERA-Interim reanalysis data indicated the importance of the deep layer of warm and moist air for WSTR events.The most significant difference between WSTR and SL events lies in their low-level convergence and lifting;for WSTR events,the low-level convergence and lifting is much shallower with comparable or stronger intensity.The trumpet-shaped topography to the north of the WSTR centers is favorable for the development of such shallow convergences in WSTR events.Results in this study will provide references for future studies to improve the predictability of WSTR.
发文机构:School of Atmospheric Sciences Key Laboratory of Regional Numerical Weather Prediction/Guangzhou Institute of Tropical and Marine Meteorology Guangdong Meteorological Observatory
关键词:warm-sectortorrentialrainfallverticalcrosssectionlow-echocentroidshallowconvergencetrumpetshapedtopography
分类号: P44[天文地球—大气科学及气象学]