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A CASE OF MESOSCALE CONVECTIVE COMPLEX EVOLVING INTO A VORTEX*
Authors:Tao Zuyu  Wang Hongqing  Bai Jie  Zhu Wenqin  Shi Dingpu and Yang Hongmei
Institution:Laboratory for Severe Storm Research, Department of Geophysics, Peking University, Beijing 100871;;Laboratory for Severe Storm Research, Department of Geophysics, Peking University, Beijing 100871;;Laboratory for Severe Storm Research, Department of Geophysics, Peking University, Beijing 100871;;Institute of Mesoscale Meteorology, Chinese Academy of Meteorological Sciences, Beijing 100081;Institute of Mesoscale Meteorology, Chinese Academy of Meteorological Sciences, Beijing 100081;Institute of Mesoscale Meteorology, Chinese Academy of Meteorological Sciences, Beijing 100081
Abstract:A case of mesoscale convective complex(MCC) which evolved into a vortex is documented in this paper.As the MCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB) of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to 250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex was visualized in the satellite images because it was located in the subtropical high where the wind field was very weak.
Keywords:mesoscale convective complex(MCC)  blackbody temperature  mesoscale vortex
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