寒潮冷堆增强的动力原因

THE DYNAMICAL CAUSE OF THE COLD DOME’S INTENSIFICATION IN THE COLD OUTBREAK PROCESS

  • 摘要: 本文利用动力学诊断方法分析了1979年11月一次东亚寒潮过程,证明500毫巴冷中心在南移过程中不断增强是由于寒潮冷空气堆中存在上升运动使空气绝热膨胀冷却所致.文中还从动力学观点解释了寒潮过程中垂直反环流的成因.指出对流层高层(300毫巴)急流核上游(入口区)和下游(出口区)存在相反的铅直环流,上游为正环流,下游为反环流.急流核两侧存在强大的正负切变涡度平流是使急流核上,下游存在性质相反的铅直环流的原因.文中近似计算了这次寒潮过程中槽后偏北急流核两侧空气的12小时二维轨迹,证明槽后偏北急流核左侧强大的正切变涡度中心及其相应的下游正涡度平流引起了寒潮冷空气堆上空质量辐散.因此在寒潮分析和预报时应注意围绕西风槽的急流分布的不均匀性,特别是300毫巴槽后偏北急流中急流核的存在及其活动对预报寒潮冷空气堆的增强是十分重要的.

     

    Abstract: In this paper,a cold outbreak process(9-11,Nov 1979) has been analysed with dynamical diagnostic method.It shows that the decrease of the temperature in the cold dome moving to south is caused not only by the diabatic cooling on the surface but also by ascending adiabatic expansion.The mass divergence above the cold dome is caused by the strong positive vorticity advection combined with the maximun vorticity on the left side of the jet core.Thus,in the proceeding of the cold outbreak forecasting,we must pay more attention to the uniform of the wind speed distribution around the trough in higher troposphere,especially the behavior of the core on the northly jet stream behind the trough.

     

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