Enhanced Decadal Warming of the Southeast Indian Ocean During the Recent Global Surface Warming Slowdown

Li Yuanlong; Han Weiqing; Zhang Lei

摘要

Abstract > The rapid Indian Ocean warming during the early‐21th century was a major heat sink for the recent global surface warming slowdown. Analysis of observational data and ocean model experiments reveals that during 2003–2012 more than half of the increased upper Indian Ocean heat content was concentrated in the southeast Indian Ocean (SEIO), causing a warming “hot spot” of 0.8–1.2?K decade ?1 near the west coast of Australia. This SEIO warming was primarily induced by the enhancements of the Pacific trade winds and Indonesian throughflow associated with the Interdecadal Pacific Oscillation's (IPO) transition to its negative phase, and to a lesser degree by local atmospheric forcing within the Indian Ocean. Large‐ensemble climate model simulations suggest that this warming event was likely also exacerbated by anthropogenic forcing and thus unprecedentedly strong as compared to previous IPO transition periods. Climate model projections suggest an increasing possibility of such strong decadal warming in future. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><abstract type =“main”xml：lang =“en”> <title type =“main”>抽象</ title> >在21世纪初期的快速印度洋变暖是最近的一个主要散热器全球表面温暖放缓。观察数据和海洋模型实验的分析表明，2003 - 2012年期间，在东南印度洋（SEIO）中，2003-2012上的上半年增加的上半年浓缩，导致0.8-1.2克的温暖“热点”为0.8-1.2？K十年澳大利亚西海岸附近的 1 </ sup>。这次SEIO变暖主要由与跨跨越太平洋振荡的（IPO）过渡到其负阶段的太平洋贸易风和印度尼西亚通风的增强，并通过当地大气迫使印度洋迫使较鲜明的程度。大集合气候模型模拟表明，与以往的IPO过渡期相比，这种变暖事件可能会因人为强制而加剧，因此前所未有的强劲。气候模型预测表明将来增加了如此强大的二层变暖的可能性。 </ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" > 著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23539/'>《Geophysical Research Letters 》</a> <b style="margin: 0 2px;">|</b><span>2017年第19期</span><b style="margin: 0 2px;">|</b> <span>共9页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Yuanlong&option=202" target="_blank" rel="nofollow">Li Yuanlong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Han Weiqing&option=202" target="_blank" rel="nofollow">Han Weiqing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Lei&option=202" target="_blank" rel="nofollow">Zhang Lei;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Atmospheric and Oceanic SciencesUniversity of ColoradoBoulder CO USA;</p> <p>Department of Atmospheric and Oceanic SciencesUniversity of ColoradoBoulder CO USA;</p> <p>Department of Atmospheric and Oceanic SciencesUniversity of ColoradoBoulder CO USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li> <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span> <a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学 ;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=decadal warming&option=203" rel="nofollow">decadal warming;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=southeast Indian Ocean&option=203" rel="nofollow">southeast Indian Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=global surface warming slowdown&option=203" rel="nofollow">global surface warming slowdown;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Indonesian throughflow&option=203" rel="nofollow">Indonesian throughflow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=anthropogenic warming&option=203" rel="nofollow">anthropogenic warming;</a> </p> <div class="translation"> 机译：Decadal变暖;东南印度洋;全球表面变暖放缓;印度尼西亚通过流量;人为变暖; 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