郑翔飚, 马红, 曾厅余. 昭通强对流天气时空分布及环流特征分析[J]. 云南大学学报(自然科学版), 2011, 33(S2): 397-401.
引用本文: 郑翔飚, 马红, 曾厅余. 昭通强对流天气时空分布及环流特征分析[J]. 云南大学学报(自然科学版), 2011, 33(S2): 397-401.
Analysis of the temporal and spatial distribution and circulation features of severe convection weather in Zhaotong[J]. Journal of Yunnan University: Natural Sciences Edition, 2011, 33(S2): 397-401.
Citation: Analysis of the temporal and spatial distribution and circulation features of severe convection weather in Zhaotong[J]. Journal of Yunnan University: Natural Sciences Edition, 2011, 33(S2): 397-401.

昭通强对流天气时空分布及环流特征分析

Analysis of the temporal and spatial distribution and circulation features of severe convection weather in Zhaotong

  • 摘要: 利用昭通市10个常规气象观测站19802008年常规观测资料和多普勒雷达资料,研究了昭通市强对流天气时空分布及环流特征.结果表明,29a中昭通强对流天气出现日数呈略减少的线性趋势变化,且存在明显的年际波动变化特征,高值与低值不规律地交替出现.强对流天气发生频次具有明显的地理和季节变化差异.强对流天气发生频繁的区域有2个,分别是东南部冰雹和雷暴的高发区和西南部大风高发区.根据强对流天气发生的天气形势将昭通强对流天气分为4种类型:高原槽型、滇黔辐合区型、切变急流型和切变冷锋型.初始回波多为西北方或南方生成移入,就地发展,减弱后移出.

     

    Abstract: Based on routine observational data of 10 conventional meteorological observation stations from 1980 to 2008 and archives of Doppler radar data in Zhaotong,the temporal and spatial distribution and circulation features of severe convection weather in Zhaotong are analyzed.The result show that Zhaotong strong convection weather in 29a presents slightly reduced linear trends,it has obvious interannual variation characteristics and irregular alternation of high value and low value.Strong convection weather occurring frequency has obvious geographical and seasonal variations.Strong convection weather occurs frequently in 2 areas:the southeast area of high hail and thunderstorm incidence,the southwest area of high gale incidence.According to the weather conditions when severe convection weather occurs, the strong convection weather in Zhaotong is divided into 4 types: plateau trough type,convergence zone type between Yunnan and Guizhou Province,shear jet type and shear cold front type.Most of initial echoes of the strong convection weather emerge in the north-west or south,they develop when move to Zhaotong and weak after they move out.

     

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