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作 者:顾天红 朱育雷 李彦霖 李力 武正敏 GU Tianhong;ZHU Yulei;LI Yanlin;LI Li;WU Zhengmin(Guizhou Meteorological Observatory,Guiyang 550002,China;Zunyi Meteorological Bureau,Zunyi 563000,China)
机构地区:[1]贵州省气象台,贵州贵阳550002 [2]贵州省遵义市气象局,贵州遵义563000
出 处:《中低纬山地气象》2021年第4期1-7,共7页Mid-low Latitude Mountain Meteorology
基 金:贵州省气象局科研业务项目:V-3θ图在贵州冰雹天气中的特征检验及应用初探。
摘 要:利用常规观测资料和MICAPS 4版的V-3θ图,选取了2018年贵州冰雹、暴雨和大雪3次转折性天气过程,对V-3θ图进行了特征检验和简单应用,得出结论如下:①V-3θ图能很好反映大气能量结构变化,其典型特征均有较好体现:超低温结构、顺滚流、θ线多折拐等;②不同转折性天气其V-3θ图特征也有所不同:冰雹天气的滚流效应最突出,暴雨、大雪依次减弱;暴雨和大雪对θsed与θ^(*)线准平行且近重合要求更高;而冰雹天气过程对对流层顶出现深厚超低温结构更为敏感;③当环流形势较弱,常规天气分析难以判断转折性天气时,可利用V-3θ图特征进行辅助预报。Using conventional observational data and the V-3θchart that comes with MICAPS 4 version,we selected three times of turning weather in Guizhou including hail,heavy rain and heavy snow,and carried out feature inspection and simple application on the V-3θchart,and the conclusions are as follows:①The V-3θchart can well reflect the changes in the energy structure of the atmosphere,and its typical characteristics are well reflected:ultra-low temperature structure,tumble flow,and multiple bending of theθline;②V-3θin different turning weather,the characteristics of the map are also different:the tumble effect of hail weather is the most prominent,with heavy rain and heavy snow sequentially weakening;heavy rain and heavy snow have higher requirements for theθsed andθ^(*)lines to be quasi-parallel and close to coincidence;while the hail weather process has a greater impact on the appearance of deep and ultra-low temperature structures in the troposphere.It is sensitive;③When the circulation situation is weak and it is difficult to judge the turning weather by conventional weather analysis,the V-3θchart feature can be used for auxiliary forecasting.
分 类 号:P456.9[天文地球—大气科学及气象学]
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