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首页> 外文期刊>Geoscience and Remote Sensing Letters, IEEE >Observational Study of the Oceanic Surface Parameters in the Eastern Indian Ocean During Two Contrasting Dipole Years 2005 and 2006
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Observational Study of the Oceanic Surface Parameters in the Eastern Indian Ocean During Two Contrasting Dipole Years 2005 and 2006

机译:东印度洋两个不同的偶极年2005年和2006年海洋表面参数的观测研究

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摘要

The Indian Ocean dipole (IOD) is one of the major interannual climate variation signals in this region through the coupled air–sea interactions. In this letter, the oceanic surface parameters in the eastern Indian Ocean during two consecutive contrasting dipole years 2005 (negative) and 2006 (positive) are examined exclusively from satellite and in situ observations. Results showed that there was sea surface temperature anomaly up to $pm 2 ^{circ}hbox{C}$ in the south eastern equatorial Indian Ocean (EEIO) during the mature phase (September–November) of the dipole. Except for the south EEIO, the south of the equator showed very high positive sea level anomaly (up to 45 cm) during the boreal fall (September–November) in 2006 under the influence of the strong positive IOD event. Similar coherent differences were observed in freshwater flux and sea surface salinity anomalies which show the large impact of these dipole events in the south EEIO box. Also, the seasonal rainfall during the northeast Indian monsoon for these two years shows substantial difference over southern India which reveals the paramount impact of IOD on the northeast monsoon rainfall.
机译:通过耦合的海-海相互作用,印度洋偶极子(IOD)是该地区主要的年际气候变化信号之一。在这封信中,仅通过卫星和实地观测资料对印度洋东部连续两个相反的偶极年2005年(负)和2006年(正)的洋面参数进行了检查。结果表明,在偶极子的成熟期(9月至11月),赤道东南部印度洋(EEIO)的海面温度异常高达$ pm 2 ^ hbox {C} $。除了南部的EEIO以外,在强烈的IOD事件的影响下,2006年的寒冬(9月至11月),赤道以南的海平面高度异常高(最大45厘米)。在淡水通量和海面盐度异常中也观察到了类似的相干差异,这表明这些偶极子事件对南部EEIO箱体的影响很大。另外,这两年印度东北季风期间的季节性降雨与印度南部显示出显着差异,这表明了IOD对东北季风降雨的最大影响。

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