The atmospheric circulation anomaly is opposite in drought years.
干旱年的环流形式与之相反。
East China summer rainfall TBO is closed with air circulation anomaly.
中国东部夏季降水tbo空间模态与大气环流异常关系密切。
The results show that there is an analogous rhythm phenomenon about six month in the evolution of circulation anomaly.
结果表明，环流异常演变过程中普遍存在着半年左右的相似韵律现象。
There was consanguineous relationship between summer rainfall anomaly in North China and continual circulation anomaly from spring to summer .
华北夏季降水异常与从春到夏的持续环流异常密切相关。
Therefore, the spring sh circulation anomaly is one of important short-term climate predictors for summer rainfall over the Yangtze River Valley.
因此，春季南半球环流异常可以作为长江中下游夏季旱涝主要短期气候预测因子。
In this paper, the index of polar vortex position is introduced. This index can preferably describe the variability of mid-high latitude circulation anomaly.
本文给出的极涡位置指数能较好地描述中高纬度环流异常的变率。
The East Asian winter monsoon anomaly has biseasonal effect on the circulation and weather in the following summer.
东亚冬季风异常可隔季影响到我国次年夏季环流和天气状况的异常。
This pattern of SSTA distribution is related to summer rainfall anomaly of North China by means of the tropical convection activity and general circulation in the middle and high latitude. iv.
这种海温异常分布型可通过夏季热带对流活动和中高纬大气环流与华北夏季降水异常产生联系。
Results show that the IOD anomaly results in anomalous atmospheric circulation, which affects the distribution of the rain belt during rainy seasons in China and the East Asian monsoon.
结果表明：印度洋海温偶极振荡异常，引起了大气环流的异常，影响了季风强度和雨带分布。
Meanwhile, the anomaly of the atmospheric circulation over the high latitude Eurasia during spring is crucial to the summer monsoon circulation and precipitation over East Asia.
而欧亚中高纬区大气环流春季异常对东亚区夏季大气环流和降水异常起着非常重要的作用。
In this paper, the seasonal changes of atmospheric circulation in the Northern Hemisphere induced by persistent anomaly of Arctic sea ice have bean examined.
本文利用全球9层15波谱模式，模拟了北极海冰后退期持续异常对北半球大气环流季节变化的影响。
In this paper, the seasonal changes of atmospheric circulation in the Northern Hemisphere induced by persistent anomaly of Arctic sea ice have bean examined.
本文利用全球9层15波谱模式，模拟了北极海冰后退期持续异常对北半球大气环流季节变化的影响。
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