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中文摘要: 该文分析了1995年7月25—31日我国东北地区中南部致洪暴雨时段Tbb场特征，并与长江中下游梅雨期致洪暴雨Tb场进行比较。结果发现，除了热带、副热带系统位置偏北且西伸外，北方致洪暴雨云带的走向，同热带、副热带云系的联系以及各系统之间的配置都和梅雨期致洪暴雨云带非常相似，这是值得注意的特点。
中文关键词: 东北地区,长江中下游地区,致洪暴雨云带,Tbb场分析
Abstract:Tbb field features of torrential rain caused flood at the midsouth in Northeast China from 25 to 31 July, 1995 were analysed and compared with that in the lower and middle reaches of the Yangtze River during the Meiyu period. The results show that both are similar in the cloud band movement, the relation with tropical or subtropical cloud systems and the allocation of the various systems, except the location of the tropical and subtropical systems was northward and westward.
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引用文本：
杨金锡,冯志娴,1996.1995年7月25—31日东北地区致洪暴雨Tbb场特征[J].气象,22(8):29-32.
,1996.Tbb Features of Torrential Rain Caused Flood in Northeast China from 25 to 31 July, 1995[J].Meteor Mon,22(8):29-32.
杨金锡,冯志娴,1996.1995年7月25—31日东北地区致洪暴雨Tbb场特征[J].气象,22(8):29-32.
,1996.Tbb Features of Torrential Rain Caused Flood in Northeast China from 25 to 31 July, 1995[J].Meteor Mon,22(8):29-32.