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首页> 外文期刊>Acta Oceanologica Sinica >A dipole mode at thermocline layer in the tropical Indian Ocean
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A dipole mode at thermocline layer in the tropical Indian Ocean

机译:热带印度洋温跃层的偶极子模式

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摘要

Temperature data at different layers of the past 45 years were studied and we found a diploe mode in the thermocline layer (DMT): anomalously cold sea temperature off the coast of Sumatra and warm sea temperature in the western Indian Ocean. First, we analyzed the temperature and the temperature anomaly (TA) along the equatorial Indian Ocean in different layers. This shows that stronger cold and warm TA signals appeared at subsurface than at the surface in the tropical Indian O-cean. This result shows that there may be a strong dipole mode pattern in the subsurface tropical Indian Ocean. Secondly we used Empirical Orthogonal Functions (EOF) to analyze the TA at thermocline layer. The first EOF pattern was a dipole mode pattern. Finally we analyzed the correlations between DMT and surface tropical dipole mode (SDM), DMT and Nino 3 SSTA, etc. and these correlations are strong.
机译:对过去45年中不同层的温度数据进行了研究,我们在温跃层(DMT)中发现了一种双峰模式:苏门答腊沿海的异常冷海温度和印度洋西部的温暖海温。首先,我们分析了赤道印度洋沿不同层的温度和温度异常(TA)。这表明在热带印度O-cean地下比在地表出现了更强的冷和暖TA信号。该结果表明,在热带印度洋地下可能存在强偶极子模式。其次,我们使用经验正交函数(EOF)来分析热跃层的TA。第一个EOF模式是偶极模式。最后,我们分析了DMT与地表热带偶极子模式(SDM),DMT和Nino 3 SSTA等之间的相关性,这些相关性很强。

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