利用闪电定位资料叠加红外辐射亮温(TBB)、雷达资料,分析了山东连续两次强对流天气过程中出现的两个中尺度对流系统(MCS)、飑线、超级单体的闪电特征,结果表明:两个MCS正地闪比重很大,强盛阶段能达一半左右。地闪多分布在TBB小于220 K...利用闪电定位资料叠加红外辐射亮温(TBB)、雷达资料,分析了山东连续两次强对流天气过程中出现的两个中尺度对流系统(MCS)、飑线、超级单体的闪电特征,结果表明:两个MCS正地闪比重很大,强盛阶段能达一半左右。地闪多分布在TBB小于220 K、对流发展旺盛且TBB梯度大的地带,地闪的分布可以很好地指示对流区;总地闪的变化与TBB极值和降水量有对应关系;对流云合并促进2016年6月14日中尺度对流系统(MCS)强烈发展,使其在初生发展阶段正闪居多并降雹。飑线中地闪多位于强回波区附近35~45 d Bz中;初生发展阶段地闪多集中于对流区,正闪多分布于云体倾斜度大的区域;成熟阶段地闪向层云区转移,多集中在低层入流边界后部,后侧入流急流上。超级单体在降雹前及降雹初期以正地闪为主,降雹前地闪频次迅速降低;降雹后,单体下沉气流增强且质心下降引发地闪猛增,最大反射率与地闪频数的变化趋势基本一致;最大反射率和回波顶高维持大值与地闪频数的骤减可以作为冰雹预测的指标。展开更多
[Objective]The aim was to analyze the first fit of rainstorm in southeast Hubei on June 9,2011.[Method]GFS reanalysis data with resolution 0.5°×0.5°,routine-observational data,the intensive observations...[Objective]The aim was to analyze the first fit of rainstorm in southeast Hubei on June 9,2011.[Method]GFS reanalysis data with resolution 0.5°×0.5°,routine-observational data,the intensive observations of automatic weather station data,satellite image as well as satellite image were used in the analysis for the process of a heavy rain on June 9-10,2011 during Meiyu in Hubei province.[Result]The heavy rainfall occurred under the favorable environmental conditions,but the single-obstruction situation during Meiyu was different from the typical double-obstruction one.The affecting systems were the trough at 45° N on 500 hPa caused the systems moving slowly in the middle and low troposphere.The strong convergence of water vapor and conditional convective instability were provided from the shear line on 700 and 850 hPa,the southwest jet flow and dry lines in the middle and low troposphere for heavy rainfall.Three rain clusters which brought heavy rainfall had the features of meso-scale β system,which came from warm and humid airflow,the tail of shear line on 700 hPa and the head of shear line on 850 hPa.Through convergence and strengthening in southeast region of Hubei Province,the ribbon structure from northeast to southwest was formed to maintain the meso-scale β system.The cloud was the direct producer of precipitation.Heavy rainfall occurred in strengthening phase of strong convection zone on Tongcheng city.[Conclusion]The study provided theoretical reference for the report of rainstorm during Meiyu period.展开更多
文摘利用闪电定位资料叠加红外辐射亮温(TBB)、雷达资料,分析了山东连续两次强对流天气过程中出现的两个中尺度对流系统(MCS)、飑线、超级单体的闪电特征,结果表明:两个MCS正地闪比重很大,强盛阶段能达一半左右。地闪多分布在TBB小于220 K、对流发展旺盛且TBB梯度大的地带,地闪的分布可以很好地指示对流区;总地闪的变化与TBB极值和降水量有对应关系;对流云合并促进2016年6月14日中尺度对流系统(MCS)强烈发展,使其在初生发展阶段正闪居多并降雹。飑线中地闪多位于强回波区附近35~45 d Bz中;初生发展阶段地闪多集中于对流区,正闪多分布于云体倾斜度大的区域;成熟阶段地闪向层云区转移,多集中在低层入流边界后部,后侧入流急流上。超级单体在降雹前及降雹初期以正地闪为主,降雹前地闪频次迅速降低;降雹后,单体下沉气流增强且质心下降引发地闪猛增,最大反射率与地闪频数的变化趋势基本一致;最大反射率和回波顶高维持大值与地闪频数的骤减可以作为冰雹预测的指标。
文摘[Objective]The aim was to analyze the first fit of rainstorm in southeast Hubei on June 9,2011.[Method]GFS reanalysis data with resolution 0.5°×0.5°,routine-observational data,the intensive observations of automatic weather station data,satellite image as well as satellite image were used in the analysis for the process of a heavy rain on June 9-10,2011 during Meiyu in Hubei province.[Result]The heavy rainfall occurred under the favorable environmental conditions,but the single-obstruction situation during Meiyu was different from the typical double-obstruction one.The affecting systems were the trough at 45° N on 500 hPa caused the systems moving slowly in the middle and low troposphere.The strong convergence of water vapor and conditional convective instability were provided from the shear line on 700 and 850 hPa,the southwest jet flow and dry lines in the middle and low troposphere for heavy rainfall.Three rain clusters which brought heavy rainfall had the features of meso-scale β system,which came from warm and humid airflow,the tail of shear line on 700 hPa and the head of shear line on 850 hPa.Through convergence and strengthening in southeast region of Hubei Province,the ribbon structure from northeast to southwest was formed to maintain the meso-scale β system.The cloud was the direct producer of precipitation.Heavy rainfall occurred in strengthening phase of strong convection zone on Tongcheng city.[Conclusion]The study provided theoretical reference for the report of rainstorm during Meiyu period.
