一次强冷空气过程阻塞形势的诊断分析  

Diagnostic Analyses on Blocking System of A Severe Cold Case

作　　者：娜仁突娅 邵明轩[1] 张瑙 

机构地区：[1]北京大学地球物理学系 [2]中国民航新疆自治区管理局,乌鲁木齐830016

出　　处：《北京大学学报（自然科学版）》2001年第3期340-347,共8页Acta Scientiarum Naturalium Universitatis Pekinensis

基　　金：高等学校重点实验室访问学者基金!资助项目

摘　　要：对 1998年 3月中旬一次高空阻塞形势下强冷空气过程进行了诊断分析 ,着重讨论强冷空气爆发前后地面反气旋活动与高空阻塞形势调整的关系。研究结果表明 ,强冷空气的爆发与乌拉尔地区阻塞形势的调整 (阻塞高压的崩溃和重建 )紧密相关。对流层下部的温度平流分析表明 ,阻塞形势的调整是由于阻塞高压上游西北方有冷空气侵入导致了阻塞高压的崩溃 ,而上游来自西南方向的强暖流则导致高压脊迅速发展 ,使阻塞高压重新建立。另外 ,70 0hPa垂直速度分布表明 。The quasi geostrophic process was diagnosed for a case of severe cold air breakout under the blocking situation during 16-18 March of 1998.The attention was focused on the relationship between the surface anticyclone and 500?hPa blocking high.The results indicate that the cold outbreak is associated with the adjustment of blocking situation in the Ural Area,i.e.the collapsing and rebuilding of the Ural Mountain blocking high.The temperature advections in the lower troposphere shown that the polar cold air invading from the northwest caused the Ural blocking high collapsed,and a new ridge developed rapidly was due to the warm advection on the southwestern side which led to the Ural blocking high rebuilt.In addition,the distribution of the vertical motion on 700?hPa shown that the surface high splitting was related to the considerable upward motion located on the southeastern part of surface high.

关 键 词：冷空气 阻塞形势 诊断 寒潮 环境 准地转理论 

分 类 号：P425.54[天文地球—大气科学及气象学]