| 1. | Inter - decadal change of sea surface temperature and its interaction between tropical pacific and indian ocean in summer and winter
印度洋海表温度年际异常的年代际变化 |
| 2. | Impacts of sea surface temperature in the tropical pacific on interannual variability of madden - julian oscillation in precipitation
热带太平洋海表温度年际变化对降水季节内振荡的影响 |
| 3. | Base on this study , the numerical forecast of 2000 ' s tropical pacific ssta has been done . it shows that it is weak la nina event in 2000
对2000年的热带太平洋海表温度作了试预报，预测结果显示2000年是弱lanina年。 |
| 4. | Finally , the possible physical mechanism by which the sst of the north pacific affecting eastern china summer rainfall was elementary discussed by numerical simulation using model ccm3
最后，运用数值模式ccm3对太平洋海表温度对东部夏季降水的影响机制进行初步研究。 |
| 5. | Almost meanwhile , the north wind anomaly brings epwp warm water to equatorial vicinity by producing north ocean flow , which causes directly nino3 sst increase
几乎与此同时，北风距平通过产生北风吹流将东太平洋暖池暖水由北向南输送至赤道附近直接导致nino3区海表温度增加。 |
| 6. | This homotopic method is an approximate analysis method , which can be more used for analyzing other behavior of the sea surface temperature anomaly of the atmosphere - ocean oscillator model
本同伦方法是近似的的解析方法，它能进一步分析海气振子的海表温度异常的其他性态。 |
| 7. | O which commenced in the latter half of 2006 finally dissipated this february . sea surface temperatures over the central and eastern tropical pacific have generally resumed normal figure 1
在2006年下半年开始发展的厄尔尼诺现象已经在今年2月消退，热带太平洋中部和东部的海表温度普遍回复正常图一。 |
| 8. | The results show that the strong winter monsoon will decrease the gradient of ssh , and change the characteristics of sst , which has influence on the sea current , especially in a shallow and closed sea area such as the south china sea
结果表明：强冬季风会减弱海面高度梯度，普遍降低黑潮区海表温度，对流场有一定的影响，尤其在南海这样的封闭海区。 |
| 9. | The waters of the western equatorial pacific are warmer than in the eastern equatorial pacific , and the difference in temperature between these two areas could produce greater temperature swings between the normal weather pattern and el nino , they wrote
西赤道太平洋的海表温度高于东赤道太平洋，这两个地区的温度差会加大地球温度在正常模式和"厄尔尼诺"之间的变化。 |
| 10. | ( 3 ) during the 1997 / 1998 el nino we find western pacific warm pool ( wpwp ) sst variation , abnormal west wind , eastern pacific warm pool ( epwp ) sst variation and abnormal north wind are associated with the nino3 index change
( 3 )在1997 1998elnino事件期间，西太平洋暖池海表温度变化及异常西风和东太平洋暖池海表温度变化及异常北风两者都与nino3指数变化密切相关。 |
