湖北农业科学 ›› 2021, Vol. 60 ›› Issue (13): 68-73.doi: 10.14088/j.cnki.issn0439-8114.2021.13.013

• 资源·环境 • 上一篇    下一篇

2018年1月湖南省两次低温雨雪冰冻过程对比分析

周慧1,2, 黄骄文1, 苏涛1, 蔡荣辉1   

  1. 1.湖南省气象台,长沙 410118;
    2.气象防灾减灾湖南省重点实验室,长沙 410118
  • 收稿日期:2020-07-03 出版日期:2021-07-10 发布日期:2021-07-26
  • 作者简介:周 慧(1973-),女,湖南沅江人,正研级高级工程师,主要从事灾害天气预报和数值预报方面的研究,(电话)13548943083(电子信箱)514446798@qq.com。
  • 基金资助:
    2019年湖南省重点研发计划项目(2019SK2161); 中国气象局创新发展专项(CXFZ2021J020)

Comparative analysis of two low temperature rain and snow freezing processes in January 2018 in Hunan province

ZHOU Hui1,2, HUANG Jiao-wen1, SU Tao1, CAI Rong-hui1   

  1. 1. Meteorological Observatory of Hunan Province,Changsha 410118,China;
    2. Hunan Key Laboratory of Meteorological Disaster Prevention and Reduction,Changsha 410118,China
  • Received:2020-07-03 Online:2021-07-10 Published:2021-07-26

摘要: 应用常规观测资料和NCEP再分析资料,对2018年1月湖南省2次低温雨雪冰冻天气过程进行了对比分析。结果显示,低温雨雪冰冻天气过程期间出现了如暴雪、冻雨、强降温、偏北大风和雷暴等多种灾害性天气;1月24—31日过程比3—8日过程影响范围广、强度强和持续时间长,主要与动力条件和热力条件存在差异有关;1月27日晚湘中以北是高架雷暴下产生的雷打雪天气现象。分析表明,500 hPa锋区、冷中心强度、850 hPa冷平流强度、地面冷高压强度及其前沿的气压梯度对初步判断冷空气的强度有较好的指示意义,700 hPa湿度和温度层结是南方雨雪相态转换的关键因子。

关键词: 低温雨雪冰冻, 对比分析, 预报着眼点, 雷打雪, 湖南省

Abstract: Based on the routine observation datas and NCEP reanalysis datas, a comparative analysis of two cold rain, snow and freezing weather processes in Hunan province in January 2018 was carried out. The results showed that there were many kinds of disastrous weather during the process, such as blizzard, freezing rain, strong cooling, northerly gale and thunderstorm. The process on January 24 to 31 had a wider range of influence, stronger intensity and longer duration than the process on 3 to 8. The dynamic condition and thermal condition was different, and it was pointed out that the thunderstorm and snowstorm occurred in the north of central Hunan province on January 27. The analysis showed that front area at 500 hPa, the strength of cold center, the cold advection intensity in 850 hPa, the intensity of cold high pressure on the ground and the pressure gradient at the front are of great significance for the determination of the intensity of cold air. Humidity and temperature stratification are the key factors for the transformation of the phase state of rain and snow in 700 hPa in south China.

Key words: cold rain, snow and freezing, comparative analysis, forecast the starting point, thunder and snow phenomenon, Hunan province

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