北方农业学报 ›› 2012, Vol. ›› Issue (6): 82-82.

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呼和浩特地区2011年11月降水异常成因分析

王晓云   

  1. 呼和浩特气象局,内蒙古呼和浩特100200
  • 出版日期:2012-12-20 发布日期:2012-12-20
  • 通讯作者: 王晓云
  • 作者简介:王晓云(1959-),女,山西阳泉人,高级工程师,主要从事气象预测预报工作。

Causality Analysis of Precipitation Anomalies in Hohhot in November 2011

WANG Xiao-yun(Hohhot Meteorological Bureau,Hohhot 010020,China)   

  • Online:2012-12-20 Published:2012-12-20

摘要: 文章对2011年11月呼和浩特地区的降水时空分布特征及成因进行了分析,结果表明:呼和浩特市地区降水较为典型,主要呈现以下3个特点:降雨大值区集中在中部土默特左旗及呼和浩特市市区,南、北部偏小;阶段性显著;极端性强。11月500hPa高度场上内蒙古中西部处于平直的西风环流中,期间多短波槽活动,南支槽活跃,副高偏西,有利于西南暖湿气流向中国北方输送。对应中国西北东部、内蒙古中部偏南降水异常偏多,究其原因与2011年9月开始的拉尼娜事件响应,及此后拉尼娜状态发展加强有关。

Abstract: In this article,the spatio-temporal characteristics and causality analysis of precipitation anomalies in November 2011 are analyzed.The results show that the precipitation feature in Hohhot is typical,mainly characterized by the following 3 features: The rainfall feature of Hohhot presents strong extremes and apparent phases,meanwhile the precipitation is mainly concentrated in the middle part of Hohhot,while South and north part is small.In November,the Middle West of Inner Mongolia lies in the flat westerlies on 500hPa height field.During that time,the shortwave trough appears frequently,the southern trough is active and the western Pacific subtropical high lies more westward,which lead to warm and wet flow coming from southwest transporting northward.Corresponding to the east part of Northwest China,the precipitation in south central Inner Mongolia is more than normal.The anomaly of rainfall is caused by a response to the La Nina event which stated in September 2011 and the development and enhancement of La Nina event ever since.

中图分类号: 

  • S161.6