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海南岛不同强弱秋汛期暴雨的环流形势和动力特征分析

冯文 吴俞 赵付竹 周玲丽

气象科学2017,Vol.37Issue(6):784-796,13.
气象科学2017,Vol.37Issue(6):784-796,13.DOI:10.3969/2016jms.0077

海南岛不同强弱秋汛期暴雨的环流形势和动力特征分析

Comparative analysis of circulation feature and dynamic structure of the rainstorms with different intensity during the autumn flood season in Hainan island

冯文 1吴俞 2赵付竹 1周玲丽1

作者信息

  • 1. 海南省气象台,海口570203
  • 2. 南京信息工程大学大气科学学院,南京210044
  • 折叠

摘要

Abstract

Daily precipitation data observed by 18 stations in Hainan and NCEP/NCAR reanalysis data are used to analyze the different intensity rainfall circulation characteristics during the autumnal flood season in Hainan.Results show that,there are many similarities in circulation configurations and precipitation distributions of the rainstorms with different intensity during autumnal flood season.The difference of the intensity and position of synoptic systems results in the precipitation discrepancy of the rainstorms during the autumnal flood season.In the strong rainstorm processes,the center of South Asia High (SAH) remain over Hainan Island,and its divergence intensity is about 2-3 times stronger than weaker rainstorm processes.At middle and lower level,Western North Pacific Subtropical High (WNPSH) is weaker and retreats from Asian continent,and tropical low-pressure system is stronger and more northern in the strong rainstorm cases.The presence of strong low-level jet in north central South China Sea(SCS) is the most significant feature of rainstorm case in autumnal flood season,but the distinct characteristics are also manifested mainly in the differentia of the shape and intensity of low level jet between different rainstorm cases.In the strong cases,the strength,length,thickness and speed gradient of jet core is much larger,and that horizontal wind circumvolve clockwise along with height,all facts are conductive to the maintenance and development of rainstorm.In addition,the jet cores of strong cases are stationary and stay over the sea near the eastern Hainan Island in the maximum precipitation day,and they fluctuate wildly in the vertical direction and wind speed.But when it comes to the weak cases,the situation is reversed,the jet cores change little in height and speed,and oscillate obviously in the east-west direction.The water vapor of the strong cases transports by three airflows:northeaster,easterly and southerly,but the vapor transportation of the weak cases is mainly due to the easterly wind.

关键词

秋汛期/暴雨/环流特征/低空东风急流

Key words

Autumnal flood season/Rainstorm/Circulation feature/Low-level easterly jet

分类

天文与地球科学

引用本文复制引用

冯文,吴俞,赵付竹,周玲丽..海南岛不同强弱秋汛期暴雨的环流形势和动力特征分析[J].气象科学,2017,37(6):784-796,13.

基金项目

国家自然科学基金资助项目(41365004) (41365004)

海南省应用技术研发与示范推广专项(ZDXM2015106) (ZDXM2015106)

海南省自然科学基金项目(413132) (413132)

气象科学

OA北大核心CSTPCD

1009-0827

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