Quantifying the Role of Oceanic Feedbacks on ENSO Asymmetry

Guan Cong; McPhaden Michael J.; Wang Fan; Hu Shijian

摘要

Abstract >The role of oceanic feedbacks in determining the asymmetry of El Ni?o–Southern Oscillation (ENSO) magnitude, spatial structure, and duration is quantified on the basis of a novel temperature variance budget. Results confirm previous studies that in the eastern Pacific, El Ni?o warm temperature anomalies are larger in magnitude than La Ni?a cold temperature anomalies mainly due to stronger positive oceanic feedbacks for El Ni?o. We find that La Ni?a cold anomalies are typically stronger than El Ni?o warm anomalies in the central Pacific with a faster growth rate for cold anomalies, due to a stronger positive thermocline feedback and weaker nonlinear damping. The thermocline feedback related to recharge oscillator dynamics plays a dominate role and leads to asymmetry in the duration of El Ni?o and La Ni?a events. In particular, the thermocline feedback becomes significantly negative during the late decaying phase of El Ni?o and speeds up its demise. </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”> <标题类型=“main”>抽象</ title> >海洋反馈在确定EL NI的不对称时的作用（ENSO ）基于新的温度方差预算来量化幅度，空间结构和持续时间。结果证实了以前的研究表明，在东太平洋，暖温度异常的幅度大于La Ni？寒冷的温度异常主要是由于EL Ni的正洋反馈更强的积极海洋反馈。我们发现La Ni？寒冷的异常通常比El Ni？o在中央的温暖异常具有更快的生长速度，这种温度较高，由于较强的正热管反馈和较弱的非线性阻尼。与充电振荡器动态相关的热线反馈起到主导作用，并在EL NI和LA NI的持续时间内导致不对称？一个事件。特别是，在EL NI的晚期衰减阶段，热控反馈变得显着负，并加速其消亡。</ p> </摘要> </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>2019年第4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=Guan Cong&option=202" target="_blank" rel="nofollow">Guan Cong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McPhaden Michael J.&option=202" target="_blank" rel="nofollow">McPhaden Michael J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Fan&option=202" target="_blank" rel="nofollow">Wang Fan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hu Shijian&option=202" target="_blank" rel="nofollow">Hu Shijian;</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>Key Laboratory of Ocean Circulation and WavesInstitute of Oceanology Chinese Academy of SciencesQingdao China;</p> <p>NOAA/Pacific Marine Environmental LaboratorySeattle WA USA;</p> <p>Key Laboratory of Ocean Circulation and WavesInstitute of Oceanology Chinese Academy of SciencesQingdao China;</p> <p>Key Laboratory of Ocean Circulation and WavesInstitute of Oceanology Chinese Academy of SciencesQingdao China;</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=ENSO asymmetry&option=203" rel="nofollow">ENSO asymmetry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic feedback&option=203" rel="nofollow">oceanic feedback;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermocline feedback&option=203" rel="nofollow">thermocline feedback;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=discharge/recharge oscillator&option=203" rel="nofollow">discharge/recharge oscillator;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zonal advective feedback&option=203" rel="nofollow">zonal advective feedback;</a> </p> <div class="translation"> 机译：ENSO不对称;海洋反馈;热控反馈;放电/充电振荡器;区间平流反馈; 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