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东北一次雪飑事件的触发机制研究

Baofeng Jiao Lingkun Ran Xinyong Shen Yanbin Qi

大气和海洋科学快报(英文版)2021,Vol.14Issue(2):13-20,8.
大气和海洋科学快报(英文版)2021,Vol.14Issue(2):13-20,8.

东北一次雪飑事件的触发机制研究

Trigger mechanism of a snow burst event in Northeast China

Baofeng Jiao 1Lingkun Ran 2Xinyong Shen 2Yanbin Qi1

作者信息

  • 1. Key Laboratory of Meteorological Disaster,Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters,Nanjing University of Information Science and Technology,Nanjing,China
  • 2. Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,China
  • 折叠

摘要

Abstract

A snow burst event characterized by brief heavy snowfall affected Northeast China and caused serious social im-pact on 26 January 2017,with the snowband generally aligned with a northeast-southwest-oriented cold front.ECMWF reanalysis data were used to diagnose the possible trigger mechanism.Results showed there were two stages:(a)an initial stage far away from the Changbai Mountains,and(b)an enhancement stage under the influ-ence of high terrain.During the initial stage,the coupling of low-level frontogenesis and a favorable convergence pattern caused strong upward motion,contributing to the release of instability.When the snowband approached the high terrain during the enhancement stage,the various instabilities were triggered by the low-level frontoge-nesis,terrain circulation,and strong wind shear associated with the low-level jet.Further,a modified Q-vector divergence including generalized potential temperature was calculated to diagnose the vertical motion.It showed that the frontogenesis terms contributed greatly to the negative Q-vector divergence along the moist isentropes,while the pseudo-vorticity terms played a role in the regions with strong wind shear associated with the low-level jet in the warm section,suggesting both were important in stimulating the ascending motion.The regions with negative Q-vector divergence had a close relationship with the vertical structure of convection,indicating the potential to track the development of the snowband in the next few hours.

关键词

雪飑/锋生/Q矢量

Key words

Snow burst/Frontogenesis/Q-vector

引用本文复制引用

Baofeng Jiao,Lingkun Ran,Xinyong Shen,Yanbin Qi..东北一次雪飑事件的触发机制研究[J].大气和海洋科学快报(英文版),2021,14(2):13-20,8.

基金项目

This study was supported by the Strategic Priority Research Pro-gram of the Chinese Academy of Sciences[grant numbers XDA17010105 and XDA20100304],the National Key Research and Development Pro-gram[grant numbers 2018YFC1507104 and 2019YFC1510400],the Key Projects of Jilin Province Science and Technology Development Plan[grant numbers 20180201035SF],and the National Natural Sci-ence Foundation of China[grant numbers 41775140 and 41790471]. ()

大气和海洋科学快报(英文版)

OACSCD

1674-2834

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