###
气象:1995,21(5):48-52
本文二维码信息
码上扫一扫!
贵州雨凇积冰过程的云层特征及环流背景
(贵州省气象科学研究所,贵阳 550002)
An Analysis on the Cloud Macro Characteristics and Circulation Background of the Severe Glaze Icing in Guizhou
摘要
图/表
参考文献
相似文献
本文已被:浏览 785次   下载 904
    
中文摘要: 雨凇形成的基本条件是地面温度在0℃以下并有过冷雨滴降至地面,严重雨凇过程的特点即是上述条件维持时间长而且有较大的过冷雨滴降水。作者使用贵阳56次探空和高空风资料,着重分析了贵州中部严重积冰过程的云内宏观热力、动力特征,发现云层厚度、云上部0℃以上暖层的存在以及云层中上部湍流强度等因子对过冷雨滴降水量有重大影响。同时,还分析了形成这种云层宏观特征的天气系统及大尺度环流背景。
Abstract:The characteristics of a severe weather of glaze icing are of the long maintenance of time and of the supercooling rainfall.By using 56 sounding and upper-wind data,the macro thermal and dynamical characteristics of cloud layer over the central part of Guizhou plateau were analysed.It was found that the cloud depth,the existence of warm(T>0℃) layer and the turbulence intensity in mid-upper cloud layer have great influence on supercooling rainfall.The synoptic system and the large scale circulation conditions for long maintenance were also discussed.
文章编号:     中图分类号:    文献标志码:
基金项目:贵州省科委年度计划资助
Author NameAffiliation
  
引用文本:
赵彩,1995.贵州雨凇积冰过程的云层特征及环流背景[J].气象,21(5):48-52.
,1995.An Analysis on the Cloud Macro Characteristics and Circulation Background of the Severe Glaze Icing in Guizhou[J].Meteor Mon,21(5):48-52.