太平洋的中央部分是北半球夏季气候变化的主要动力源。
赤道西大平洋暖池海表温度(SST)对西风爆发(WWB)的响应是WWB与ENSO相互作用的一个重要环节。
The responses of sea surface temperature (SST) in the western equatorial Pacific warm pool to the westerly wind bursts (WWBs) play an important role in the relationship between WWB and ENSO.
在赤道西太平洋暖池，温度的纬向对流有很大的贡献。
The western Pacific warm pool is mainly contributed by zonal temperature advection.
西太平洋暖池区SST的变化，与南印度洋西风漂流区、赤道北印度洋存在显著的正相关。
It is also found that the variation of WEWP SST is positively correlated with the equatorial northern Indian Ocean and the west wind drift of the southern Indian Ocean.
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