文中研究了江淮流域特大洪涝的环流特征。
Characteristics of the atmospheric general circulation during the catastrophic floods over the Changjiang-Huaihe River Valley (CHRV) are investigated.
来自孟加拉湾和南海的暖湿气流为江淮流域提供了充足的水汽。
The warm moist flow from the Bay of Bengal and the South China Sea provided the rainstorm sufficient moisture.
结果表明：江淮流域夏季降水与前期地面气温的东亚纬向海陆热力差异相关；
The results show that the summer precipitation in Jianghuai valley is related to zonal sea-land thermal contrast in East Asia of early days surface air temperature.
通过一次江淮流域暴雨天气过程的分析，发现在对流层低层存在一种中间尺度扰动。
Using the analyses of weather process of an heavy rainfall system, it is found that there is a mesoscale disturbance in the lower troposphere over Yangzi-Hwai valley.
利用一个具有门限的非线性随机动力气候模式对中国东部江淮流域的降水进行了分析。
This paper applies a non linear stochastic dynamic model with threshold to analyze the rainfall in the Yangtze and Huaihe river basins of east China.
积雪的增加会明显减弱亚洲夏季风的强度，使华南的降水减少，江淮流域的降水增多。
Increasing snow cover will obviously decrease the strength of Asia summer monsoon and the precipitation of South China and increase the precipitation of the Changjiang River valley.
在春季AAO偏强的情况下，1976年之前，长江以南地区和华北地区降水偏多，江淮流域降水偏少；
When the AAO in boreal spring was stronger before 1976, there was more rainfall in the south of the Yangtze River and north China and less rainfall in the Yangtze-Huaihe River valley.
试验结果显示，该模式能够合理地模拟出1991年夏季东亚地区的逐日降水过程，特别是在江淮流域发生的异常降水事件。
The model can reasonably reproduce the daily precipitation events over East Asia for the summer of 1991, especially in the Yangtze-Huaihe valley where the anomalous rainfall occurred.
结果表明：STPNA（海温的太平洋北美遥相关型）指数距平累积和与江淮流域夏季降水有密切的相关，与全国雨带的类型也有较好的联系。
The results indicate that there is better relationship between the departure accumulation of the index STPNA (PNA teleconnection pattern of the North Pacific SST) and flood season rainfall in china.
汉代以后巢湖流域文化衰落是安徽江淮地区考古研究中一个非常引人注目的现象。
The culture decline of Chaohu Lake Basin after the Han Dynasty is a remarkable archaeological phenomenon in Jianghuai region, Anhui Province.
西周以前他们亦生活在江淮平原和汉水流域，后来由于战乱才逐渐西迁到了川黔滇之交地区。
Before the Western Zhou dynasty, they also lived on the middle and lower Yangtze valley plains and in the valley of the Han River.
西周以前他们亦生活在江淮平原和汉水流域，后来由于战乱才逐渐西迁到了川黔滇之交地区。
Before the Western Zhou dynasty, they also lived on the middle and lower Yangtze valley plains and in the valley of the Han River.
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