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Connection between interannual variability of the western Pacific and eastern Indian Oceans in the 1997 -- 1998 El Nino event

机译:1997-1998年厄尔尼诺事件中西太平洋和印度洋东部的年际变化之间的联系

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摘要

In this paper, the sea surface height and the heat content of the upper ocean are analyzed to retrieve the relationship of interannual variabilities between the tropical western Pacific and eastern Indian Oceans during the 1997-- 1998 El Nino event, I n the prophase of this El Nino, the negative sea level anomalies (SLA) occurred in the tropical western Pacific (TWP) firstly, and then appeared in the tropical eastern Indian Ocean (TEI). The negative heat content anomalies (HCA) emerged in the TWP befo re this El Nino burst while the SLA signals developed over there During the mature stage of this El Nino, two kinds of signals in the TWP and TEI turned to be the maximum negative sequently Due to the connected interannual adjustment between the TEI and TWP, we adopted a method to estimate the Indonesian Throughflow (ITF) transport by calculating the HCA budget in the TEI.The indirect estimation of the ITF was comparable to the observation values. Therefore, the anomalies in the TEI had been proved as a dvecting from the TWP through the ITF during the 1997-1998 El Nino.
机译:本文分析了1997--1998年厄尔尼诺事件期间热带西太平洋和印度洋东部的海平面高度和上层海洋的热量,以求出它们之间的年际变化关系。厄尔尼诺现象是,负海平面异常(SLA)首先发生在热带西太平洋(TWP),然后出现在热带东部印度洋(TEI)。在El Nino爆发之前,TWP中出现了负热含量异常(HCA),而那边出现了SLA信号。在El Nino的成熟阶段,TWP和TEI中的两种信号依次变为最大负值由于TEI和TWP之间的年度相互调整,我们采用了一种通过计算TEI中的HCA预算来估算印尼流量(ITF)输送的方法,ITF的间接估算与观测值相当。因此,在1997-1998年厄尔尼诺现象期间,TEI的异常被证明是通过TWP通过ITF发生的。

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