The sea surface temperature (SST) over equatorial eastern Pacific was the most important force factor for the seasonal and annual variation of east Asian monsoon circulation.
冬季赤道东太平洋海温变化是冬、夏东亚环流季节以及年际变化的一个重要外强迫因子。
In this paper the climatic features of the sea fog along the coast of South China are analyzed, and the relationship between the sea fog and the eastern equatorial Pacific SST is revealed.
本文分析了华南沿海海雾的气候特征及其与赤道东太平洋海温的关系。
During SST raise stage in the equatorial central and eastern Pacific and North Pacific westerly drift region, serious droughts and floods easily happen in the North China Plane, respectively.
在赤道中东太平洋海温与北太平洋西风漂流区海温处于明显正距平阶段 ，华北平原地区易分别发生严重干旱与雨涝。
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