主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报

• 简报 • 上一篇    下一篇

2010年2月24日沈阳地区冻雨成因分析

方纯纯   

  1. 中国民航东北地区空中交通管理局气象中心,辽宁 沈阳110043
  • 收稿日期:2010-08-16 修回日期:2010-10-29 出版日期:2010-12-29 发布日期:2010-12-29

Analysis of formation of freezing rain on February 24, 2010 in Shenyang, Liaoning province

FANG Chun-chun   

  1. Meteorological Center, Civil Aviation Air Traffic Management Bureau in Northeast China, Shenyang 110043, China
  • Received:2010-08-16 Revised:2010-10-29 Online:2010-12-29 Published:2010-12-29

摘要: 利用NCEP的全球数据同化系统(GDAS)1°×1°分析资料、NOAA的2.5°×2.5°全球格点资料和气象观测资料等,对2010年2月24日沈阳地区大范围冻雨灾害天气过程进行分析。结果表明:冻雨发生前期,沈阳地区的明显增温是导致大范围雨雪冰冻灾害的重要原因;925—750 hPa存在的t≥0℃温厚暖层是冻雨形成的必要条件;西南气流的建立有利于大量暖湿空气向东北地区输送,并决定了低温冰冻灾害发生的区域。中层温厚暖层的建立与破坏时间对冻雨的预报具有一定的指示意义。

关键词: 冻雨, 高低空环流, 中层暖层结构, 西南气流, 增温

Abstract: Based on 1° × 1° global data assimilation system (GDAS) data from NCEP, 2.5° × 2.5° global grid data from NOAA and meteorological observational data, the weather process of freezing rain on February 24, 2010 in Shenyang region was analyzed. The results show that obvious warming prior to the freezing rain is the important reason causing freezing rain disaster in Shenyang region. Warm and deep layer between 925 hPa and 750 hPa in which temperature is equal or greater than 0 ℃ is the necessary condition for the formation of freezing rain. Southwest airflow contributes to the transmission of warm and moist air to the northeast region, and it could determine the range of freezing disaster occurrence. The time of establishment and destruction of warm and deep middle layer is indicative to forecast of freezing rain.

中图分类号: