Abstract:The large-and meso-scale features of a subtropical rainband which caused thunderstorms over western Japan (*33N/130E) in 25*27 July 1981 are studied. This case aroused our interest because the convective activities persisted for about three days in the west side of a slow-moving ridge.Radar observations showed a persistent convective echo band of *800km length extending in NNW*SSE direction. This echo band was not accompanied with front-like strong thermal gradient. Satellite IR imageries showed that the rainb… Show more
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