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。
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。
The northerly component of the winter monsoon anomaly makes the anomalous cyclone over the western Pacific not exist and the East Asian summer monsoon becomes stronger.
在异常的冬季风偏北风分量强迫下，西太平洋上形成的偏差气旋环流在夏季已不存在，这时东亚夏季风反而增强。
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