Yan Zhihui, Tian Hua. Causality analysis of a heavy rain process over middle and lower reaches of Changjiang River in June 1998. J Appl Meteor Sci, 2002, 13(6): 680-687.
Citation: Yan Zhihui, Tian Hua. Causality analysis of a heavy rain process over middle and lower reaches of Changjiang River in June 1998. J Appl Meteor Sci, 2002, 13(6): 680-687.

CAUSALITY ANALYSIS OF A HEAVY RAIN PROCESS OVER MIDDLE AND LOWER REACHES OF CHANGJIANG RIVER IN JUNE 1998

  • Received Date: 2001-04-25
  • Rev Recd Date: 2001-11-05
  • Publish Date: 2002-12-31
  • A numerical experiment on a heavy rain process occurred in the last dekad of June in 1998 is conducted by means of the limited area prediction model of the National Meteorological Center. The formation causes of the process are discussed through analyzing the winds, water vapor, vertical velocity and other elements. The results show that the main synoptic scale weather systems causing the heavy rain are the Southwest low-level jet and a shear line between dry air from north and warm and moist air from /southwest in the middle and lower reaches of the Changjiang River. The mesoscale weather systems moving along the shear line play a very important role in precipitation reinforcement
  • [1]
    闫之辉,郭肖容,赵俊英,等.一个载水预报模式的业务预报应用试验.应用气象学报,1999,10(4):453-461. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19990487&flag=1
    [2]
    国家气象中心,国家气候中心.1998中国大洪水与天气预报.北京:气象出版社,1999.65-68.
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    • Received : 2001-04-25
    • Accepted : 2001-11-05
    • Published : 2002-12-31

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