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INTRACLOUD LIGHTNING DISCHARGES IN THE LOWER PART OF THUNDERCLOUD
作者姓名:刘欣生  叶宗秀  邵选民  王才伟  言穆弘  郭昌明
作者单位:Lanzhou Institute of Plateau Atmospheric Physics Academia Sinica,Lanzhou,Lanzhou Institute of Plateau Atmospheric Physics,Academia Sinica,Lanzhou,Lanzhou Institute of Plateau Atmospheric Physics,Academia Sinica,Lanzhou,Lanzhou Institute of Plateau Atmospheric Physics,Academia Sinica,Lanzhou,Lanzhou Institute of Plateau Atmospheric Physics,Academia Sinica,Lanzhou,Lanzhou Institute of Plateau Atmospheric Physics,Academia Sinica,Lanzhou
基金项目:This work was supported by the National Natural Science Foundation of China.
摘    要:From analysis of observational data of thunderstorms in Gansu,China,it was deduced that the electricstructure of thunderclouds in this region is often positive charge in the upper,main negative in the middlelayer and another positive charge,large in magnitude and extensive in dimension,in the lower part.Intra-cloud discharges often take place between the main negative charge and lower positive charge instead of upper.Case analysis of 6 intracloud discharges in two storms on August 3 and 4,1986 shows that the centers of thesedischarges and the dipole moments destroyed were at the altitude of 3.8—6 km msl(7.6—-13.5℃)and 18—40 C km,respectively.

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