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为了检验第三代 ＩＡＰ／ＬＡＳＧ全球海洋环流模式在模拟 ２０世纪 ８０年代热带太平洋年际变化方面特别是圆 Ｎｉｎｏ和 Ｌａ Ｎｉｎａ事件的能力，作者使用了三种风应力资料强迫该模式。然后，将模拟的海温同ＮＣＥＰ海洋同化资料相比较。分析表明，在赤道附近，模式对风应力的响应在 ＳＳＴ分布。温跃层的描绘以及突出Ｅｌ Ｎｉｎｏ和 Ｌａ Ｎｉｎａ事件方面同 ＮＣＥＰ海洋同化资料有许多共同点。然而，在描绘１０°Ｎ以北和１０°Ｓ以南的ＳＳＴ异常以及描写季节循环方面，响应是不够精确的。另外，模拟的温度异常滞后于ＮＣＥＰ海洋同化数据两个月左右
To test the ability of the third generation IAP / LASG global ocean circulation model to model the interannual variability of the tropical Pacific in the 1980s, especially the round Nino and La Nina events, the authors used three wind stress data to force the model. The simulated SST is then compared with the NCEP ocean assimilation data. The analysis shows that in the vicinity of the equator, the mode response to wind stress is distributed in the SST. The thermocline characterization and highlighting El Nino and La Nina events have much in common with NCEP data on ocean assimilation. However, the response is inaccurate in characterizing SST anomaly north of 10 ° N and south of 10 ° S, as well as characterizing seasonal cycles. In addition, simulated temperature anomalies lag behind NCEP ocean assimilation data for about two months