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一次北上江南气旋的结构特征与演变机理分析

郭达烽 熊秋芬 张昕

气象2017,Vol.43Issue(4):413-424,12.
气象2017,Vol.43Issue(4):413-424,12.DOI:10.7519/j.issn.1000-0526.2017.04.003

一次北上江南气旋的结构特征与演变机理分析

Structure and Mechanism Analysis of One Jiangnan Cyclone with Northern Track

郭达烽 1熊秋芬 2张昕2

作者信息

  • 1. 江西省气象台,南昌330046
  • 2. 中国气象局气象干部培训学院,北京100081
  • 折叠

摘要

Abstract

The structure and mechanism of a Jiangnan cyclone with a northern track that occurred during 10-13 May 2014 was analyzed by using conventional observations,NCEP 1°× 1° reanalysis data and water vapor images from FY-2E.The results are as follows:(1) The distribution of pressure and rainfall areas is similar to the output of Shapiro-Keyser conceptual model.(2) The Jiangnan cyclone occurred under the weather situation of the divergence at 250 hPa,and trough merger and ridge development downward at 500 hPa.(3) The weak warm core existed close to the low center under 850 hPa,but there was no back-bent warm front as Shapiro-Keyser conceptual model showed.(4) When the positive relativity vorti-city tilted westward with height,the cold frontal zoneintensified in the western side of surface cyclone and the positive relativity vorticities in the upper troposphere strengthened,the cyclone was rapidly deepening;when the positive relative vorticities at different levels were nearly vertically overlapped and the cold frontal zone in the low troposphere weakened,the cyclone developed slowly.(5) Heavy rain was caused by warm and moisture air,strong upward vertical volecity with two secondary circulation crossing the warm front.(6) It was also found by equation that surface cyclone hardly developed without upward vertical velocity at the initial stage,but it moved rapidly toward northeast as the result of warmer advection and larger differential vorticity advection between the upper-level and low-level troposphere downstream during cyclogenesis.Then surface cyclone was intensified rapidly by srtong upward vertical velocity,but it moved slowly due to the less warm advection and differential vorticity advection.Surface cyclone was slowly deepening due to weakly upward vertical velocity,and it moved more slowly because of the weakly warm advection and differential vorticity advection.

关键词

江南气旋/暖核/相对涡度/成因/ω方程

Key words

Jiangnan cyclone/warm core/relative vorticity/mechanism/ω-equation

分类

天文与地球科学

引用本文复制引用

郭达烽,熊秋芬,张昕..一次北上江南气旋的结构特征与演变机理分析[J].气象,2017,43(4):413-424,12.

基金项目

国家自然科学基金项目(91637105和41475041)及中国气象局预报员专项(CMAYBY2015-039、CMAYBY2016-092和CMAYBY2016-093)共同资助 (91637105和41475041)

气象

OA北大核心CSCDCSTPCD

1000-0526

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