杨有仁, 和卫东. 丽江市强对流天气背景条件研究[J]. 云南大学学报(自然科学版), 2012, 34(S2): 357-363.
引用本文: 杨有仁, 和卫东. 丽江市强对流天气背景条件研究[J]. 云南大学学报(自然科学版), 2012, 34(S2): 357-363.
YANG Youren, HE Weidong. Lijiang strong convection weather occurring background analysis[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S2): 357-363.
Citation: YANG Youren, HE Weidong. Lijiang strong convection weather occurring background analysis[J]. Journal of Yunnan University: Natural Sciences Edition, 2012, 34(S2): 357-363.

丽江市强对流天气背景条件研究

Lijiang strong convection weather occurring background analysis

  • 摘要: 选取2006年到2011年丽江市境内发生的76个强对流暴雨和冰雹个例,从影响的天气系统、水汽条件、大气层结结构、能量条件和中尺度水汽、急流特征等5个方面进行了分析,得到了如下主要结论:一是对流层中层偏北气流、中低层切变低涡、地面冷空气是强对流暴雨或冰雹形成的主要天气系统,夏秋季西太平洋副热带高压西伸或东退过程中,在其边缘也有可能出现强对流暴雨或冰雹天气;二是大部分强对流暴雨或冰雹形成前,气层无明显不稳定特征,08时的对流不稳定度对其指示作用不显著;三是强对流暴雨形成前,中低层有深厚的高湿度层,而且有较好的水汽输送,而冰雹形成前,上干下湿的层结特征明显;四是对流层急流对丽江境内强对流暴雨或冰雹的形成作用不大,指示性较差;五是要重视更高层次垂直风切变的分析.

     

    Abstract: From 2006 to 2011 in Lijiang City,the 76 strong convection rainstorm and hail process,from the effects of weather system,the water vapor condition,atmospheric stratification structure,energy conditions and mesoscale moisture,jet characteristics in 5 aspects to carry on the analysis,obtained the following conclusions:one is the middle troposphere,northerly flow low level shear vortex,surface cold air is the strong convection rainstorm and hail formation of the main weather systems in summer and autumn,West Pacific subtropical high extended West or East annealing process,at its edges may also occur in the strong convection rainstorm and hail;two is the majority of the strong convection rainstorm and hail formation,gas reservoir without obvious stable characteristic,08 when the convective instability of the indicating no significant effect;the three is the strong convection rainstorm formation,low layer deep high moisture layer,and has good water vapor transmission,and hail formation,dry wet stratification characteristics;four is the tropospheric jet streams in Lijiang strong convective heavy rain or hail formation is indicative of poor; Five is to attach importance to higher levels of vertical shear of wind analysis.

     

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