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移出高原后长生命史高原低涡在不同移动路径下的大尺度环流特征及差异

师锐 何光碧

气象2018,Vol.44Issue(2):213-221,9.
气象2018,Vol.44Issue(2):213-221,9.DOI:10.7519/j.issn.1000-0526.2018.02.001

移出高原后长生命史高原低涡在不同移动路径下的大尺度环流特征及差异

Comparison Analysis of Circulation Features of Different Moving Tracks of Long-Life-Cycle Plateau Vortexes Moving out of the Plateau

师锐 1何光碧2

作者信息

  • 1. 成都高原气象研究所,成都610072
  • 2. 四川省气象台,成都610072
  • 折叠

摘要

Abstract

Using the upper-air observation data and the corresponding daily average NCEP reanalysis data,this paper first statistically analyzed the plateau vortexes which could live 3 days or longer after moving out of Tibetan Plateau in summer from 2000 to 2010.According to their different moving track,the vortexes were divided into three groups which are moving eastward,northeastward and southeastward.The results show that in July long-life-cycle vortexes moving out of the plateau move eastward far more than northeastward and southeastward,and the vortexes moving southeastward are more than those moving northeastward.However,in August,the vortexes moving southeastward are far more than those moving northeastward and eastward.Then by selecting the cases of different moving tracks,we analyzed the general circulation in the mid-upper troposphere,pointing out the common features and differences of the general circulation and temperature advection at 500 hPa and the circulation at 200 hPa.The findings indicate that the position and shape of West Pacific subtropical high influence the long-life-cycle plateau vortex moving out of the plateau at 500 hPa significantly,and the strength of the subtropical high decreases in the order of the tracks moving eastward,northeastward and southeastward.The southeastward track over the Indian-Burma Region is affected by monsoon depression while the eastward and northeastward tracks are affected by the Indian monsoon trough,namely to south of 25°N of the southeastward track there is a rela tively lower geopotential height which is favorable for the plateau vortex to move southward.Under the 200 hPa circulation background,the eastern end of the 1252 dagpm South Asia high is by west in the order of eastward,northeastward and southeastward tracks.For the eastward track cases,the eastern end of South Asia high is obviously by east,causing the westerly flow to guide the plateau vortex to move eastward.And for the southeastward track cases,the northern boundary of the South Asia high over the Tibetan Plateau and north-west flow after high trough at 110°E guide the plateau vortex to move southeastward.Cold air is also an important factor for the development of these long-life-cycle plateau vortexes.The corresponding relationship exists between the moving direction of the temperature advection zone and the moving tracks of long-life-cycle plateau vortexes moving out of the plateau.

关键词

长生命史高原低涡/大尺度环流/温度平流/南亚高压

Key words

long-life-cycle plateau vortex/large-scale circulation/temperature advection/South Asia high

分类

天文与地球科学

引用本文复制引用

师锐,何光碧..移出高原后长生命史高原低涡在不同移动路径下的大尺度环流特征及差异[J].气象,2018,44(2):213-221,9.

基金项目

国家自然科学基金重点项目(91337215)、国家重点基础研究发展计划(973计划)(2012CB417202)、国家自然科学基金面上项目(41275051)和中国气象局预报员专项(CMAYBY2017-063)共同资助 (91337215)

气象

OA北大核心CSCDCSTPCD

1000-0526

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