首页|黔南州冰雹天气环流特征分析

黔南州冰雹天气环流特征分析

扫码查看
[目的]为了建立黔南地区冰雹发生前天气背景流型配置和T-logP图形态本地化天气概念模型.[方法]选取2006-2022年黔南30次降雹事件,运用天气学分析方法对常规高空、地面气象资料进行研究分析.[结果]以地面流型为主、高低空流型为辅,黔南地区冰雹事件发生前天气类型可分为热低压辐合型、高架雷暴型和冷锋低槽(切变)型3类.[结论]3类天气分型特征如下:(1)热低压辐合型降雹高频次区域为黔南中北部,高架雷暴型降雹高频次区域为黔南中部,冷锋低槽(切变)型降雹高频次区域为黔南中南部;(2)T-logP图形态共有4种,分别为漏斗无梭形、无漏斗梭形、小漏斗梭形、大漏斗梭形,热低压辐合型以大漏斗梭形为主,高架雷暴型以漏斗无梭形为主,冷锋低槽(切变)型以无漏斗梭形为主.
Analysis of Circulation Characteristics of Hail Weather in Qiannan
Based on 30 hail events in Qiannan Prefecture from 2006 to 2022,this paper analyzes the corresponding conventional upper-air and surface meteorological data by means of synoptic analysis method to establish a localized weather concept model regarding the configuration of weather background flow types and T-logP patterns prior to hail occurrence in Qiannan Prefecture.The findings indicate that the synoptic patterns preceding hail events in Qiannan Prefecture can be categorized into three types:thermal low-pressure convergence type,elevated thunderstorm type,and cold-front low-trough(shear)type.The surface flow pattern is dominant,supplemented by high and low air flow patterns.The characteristics of the three types of synoptic patterns are as follows:(1)The central and northern parts of Qiannan Prefecture exhibits a higher frequency of hail occurrences under the thermal low-pressure convergence type,the central part tends to have more frequent hail events under the elevated thunderstorm type,and the central and southern parts encounter increased hail frequencies under the cold-front low-trough(shear)type.(2)There are four T-logP patterns,including funnel-free shuttle pattern,no funnel shuttle pattern,small funnel shuttle pattern,and large funnel shuttle pattern.The thermal low-pressure convergence type is primarily featured with a large funnel shuttle pattern,the elevated thunderstorm type with a funnel-free shuttle pattern,and the cold-front low-trough(shear)type with a no funnel shuttle pattern.

hailsynoptic circulationT-logP

黄麟媛、罗喜平、罗雄、赵杰、莫乙冬

展开 >

贵州省黔南布依族苗族自治州气象局,贵州 都匀 558000

贵州省气候中心,贵州 贵阳 550002

贵州省气象台,贵州 贵阳 550002

冰雹 天气环流 T-logP图

贵州省气象局研究型业务关键技术攻关团队贵州省科技计划项目贵州省科技计划项目

GGTD-202208黔科合支撑[2022]一般206黔科合支撑[2023]一般194

2024

中低纬山地气象
贵州省气象学会

中低纬山地气象

影响因子:0.33
ISSN:2096-5389
年,卷(期):2024.48(3)
  • 8