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首页|期刊导航|大气科学|2011~2012年冬季欧亚大陆低温严寒事件与平流层北极涛动异常下传的影响

2011~2012年冬季欧亚大陆低温严寒事件与平流层北极涛动异常下传的影响

兰晓青 陈文

大气科学2013,Vol.37Issue(4):863-872,10.
大气科学2013,Vol.37Issue(4):863-872,10.DOI:10.3878/j.issn.1006-9895.2012.12061

2011~2012年冬季欧亚大陆低温严寒事件与平流层北极涛动异常下传的影响

Strong Cold Weather Event over Eurasia during the Winter of 2011/2012 and a Downward Arctic Oscillation Signal from the Stratosphere

兰晓青 1陈文2

作者信息

  • 1. 中国科学院大气物理研究所季风系统研究中心,北京100190
  • 2. 中国科学院研究生院,北京100049
  • 折叠

摘要

Abstract

The circulation evolution and possible causes of a severe cold event over the Eurasian continent during the winter of 2011/2012 were investigated with the NCEP-NCAR reanalysis data.Strong cold anomalies covering most of Europe,Mongolia,and northeastern China began in late January 2012 and lasted for about 3 weeks.Analysis results indicate that this cold event coincided with the phase of the Arctic Oscillation (AO) changing from positive to negative,which implied a possible impact of the AO.Before this AO phase change,a minor warming occurred in the stratosphere caused by an anomalous upward propagation of planetary waves.The polar night jet then decelerated and the AO changed its sign in the stratosphere.Within 2-3 weeks,the stratospheric AO signal gradually propagated downward and accordingly the tropospheric AO evolved into the negative phase.Thus,a strong Ural blocking high developed,and cold air invaded Europe and East Asia from the polar region,which induced the decreasing temperature there.Our results suggest that improvements can be made in predicting severe winter cold events over Eurasia by taking into account the stratospheric circulation anomaly.

关键词

冬季低温严寒事件/北极涛动/平流层环流/行星波

Key words

Severe cold event during winter/ Arctic Oscillation/ Stratospheric circulation/ Planetary wave

分类

天文与地球科学

引用本文复制引用

兰晓青,陈文..2011~2012年冬季欧亚大陆低温严寒事件与平流层北极涛动异常下传的影响[J].大气科学,2013,37(4):863-872,10.

基金项目

国家重点基础研究发展规划项目 2010CB428603,国家自然科学基金资助项目 41025017 ()

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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