Zhang Xiaoling, Tao Shiyan, Zhang Qingyun. An analysis on development of meso-β convective system along Meiyu front associated with flood in Wuhan in 20-21 July 1998. J Appl Meteor Sci, 2002, 13(4): 377-396.
Citation: Zhang Xiaoling, Tao Shiyan, Zhang Qingyun. An analysis on development of meso-β convective system along Meiyu front associated with flood in Wuhan in 20-21 July 1998. J Appl Meteor Sci, 2002, 13(4): 377-396.

AN ANALYSIS ON DEVELOPMENT OF MESO-Β CONVECTIVE SYSTEM ALONG MEIYU FRONT ASSOCIATED WITH FLOOD IN WUHAN IN 20-21 JULY 1998

  • Received Date: 2001-01-09
  • Rev Recd Date: 2001-04-30
  • Publish Date: 2002-08-31
  • On 21 July 1998 a flash flood associated with a meso-β convective system occurred in Wuhan, producing 88 mm rainfall in an hour. A diagnostic study of the genesis and development of the mesoscale convective system (MCS) is presented. The conclusions are as follows: (1) The flash flood occurred during the rapidly developing stage of the MCS. (2) There was aboundent moisture gathered in the lower troposphere and the atmosphere was nearly saturated with a big store of convective available potential energy (CAPE). (3) The MCS became nearly stationary in the vicinity of Wuhan after formed and a great amount of rainfall was accumulated in this area.
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    • Received : 2001-01-09
    • Accepted : 2001-04-30
    • Published : 2002-08-31

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