Role of interannual        <fc xmlns='http://www.wiley.com/namespaces/wiley'>K</fc>K        elvin wave propagations in the equatorial        <fc xmlns='http://www.wiley.com/namespaces/wiley'>A</fc>A        tlantic on the        <fc xmlns='http://www.wiley.com/namespaces/wiley'>A</fc>A        ngola        <fc xmlns='http://www.wiley.com/namespaces/wiley'>B</fc>B        enguela        <fc xmlns='http://www.wiley.com/namespaces/wiley'>C</fc>C        urrent system

Imbol Koungue Rodrigue Anicet; Illig Serena; Rouault Mathieu

摘要

Abstract >The link between equatorial Atlantic Ocean variability and the coastal region of Angola‐Namibia is investigated at interannual time scales from 1998 to 2012. An index of equatorial Kelvin wave activity is defined based on Prediction and Research Moored Array in the Tropical Atlantic (PIRATA). Along the equator, results show a significant correlation between interannual PIRATA monthly dynamic height anomalies, altimetric monthly Sea Surface Height Anomalies (SSHA), and SSHA calculated with an Ocean Linear Model. This allows us to interpret PIRATA records in terms of equatorial Kelvin waves. Estimated phase speed of eastward propagations from PIRATA equatorial mooring remains in agreement with the linear theory, emphasizing the dominance of the second baroclinic mode. Systematic analysis of all strong interannual equatorial SSHA shows that they precede by 1–2 months extreme interannual Sea Surface Temperature Anomalies along the African coast, which confirms the hypothesis that major warm and cold events in the Angola‐Benguela current system are remotely forced by ocean atmosphere interactions in the equatorial Atlantic. Equatorial wave dynamics is at the origin of their developments. Wind anomalies in the Western Equatorial Atlantic force equatorial downwelling and upwelling Kelvin waves that propagate eastward along the equator and then poleward along the African coast triggering extreme warm and cold events, respectively. A proxy index based on linear ocean dynamics appears to be significantly more correlated with coastal variability than an index based on wind variability. Results show a seasonal phasing, with significantly higher correlations between our equatorial index and coastal SSTA in October–April season. </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 xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”> <标题类型=“main”>抽象</ title> >在1998年至2012年的持续时间尺度上调查了赤道大西洋变异性和安哥拉纳米比亚沿海地区之间的联系。基于热带大西洋中的预测和研究系泊阵列来定义赤道凯尔文波浪活性指标（ pirata）。沿赤道沿着赤道，结果在依际Pirata每月动态高度异常（Altimetric每月海面高度异常（SSHA）和SSHA用海洋线性模型计算的显着相关性。这使我们能够在赤道开尔文波中解释PiRata记录。从Pirata赤道系泊的东方传播的估计速度仍然与线性理论一致，强调了第二个律键模式的主导地位。对所有强大持续赤道SSHA的系统分析表明，他们在非洲海岸沿着1-2个月的极端持续的海面温度异常，这证实了安哥拉 - 孟加拉国当前系统中主要温暖和冷的事件的假设是由海洋迫使的赤道大西洋的大气互动。赤道波动态处于其发展的起源。 Western赤道大西洋力量赤道沉船和Upwwelling Kelvin波的风异常沿着赤道向东传播，然后沿着非洲海岸引发极端温暖和冷的事件。基于线性海洋动力学的代理指数似乎与基于风变性的索引的沿海可变性显着更大。结果显示季节性阶段，在4月至4月季节的赤道指数和沿海SSTA之间具有显着提高的相关性。</ 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-34643/'>《Journal of Geophysical Research, C. Oceans: JGR》</a> <b style="margin: 0 2px;">|</b><span>2017年第6期</span><b style="margin: 0 2px;">|</b><span>共19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=Imbol Koungue Rodrigue Anicet&option=202" target="_blank" rel="nofollow">Imbol Koungue Rodrigue Anicet;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Illig Serena&option=202" target="_blank" rel="nofollow">Illig Serena;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rouault Mathieu&option=202" target="_blank" rel="nofollow">Rouault Mathieu;</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 OceanographyMARE Institute University of Cape TownCape Town South Africa;</p> <p>Department of OceanographyMARE Institute University of Cape TownCape Town South Africa;</p> <p>Department of OceanographyMARE Institute University of Cape TownCape Town South Africa;</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=equatorial Kelvin waves&option=203" rel="nofollow">equatorial Kelvin waves;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Benguela Ni?os&option=203" rel="nofollow">Benguela Ni?os;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tropical Atlantic&option=203" rel="nofollow">tropical Atlantic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=PIRATA&option=203" rel="nofollow">PIRATA;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=upwelling&option=203" rel="nofollow">upwelling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Benguela Current&option=203" rel="nofollow">Benguela Current;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Angola Current&option=203" rel="nofollow">Angola Current;</a> </p> <div class="translation"> 机译：赤道凯尔文波;孟加拉国？卫生;os;热带大西洋;Pirata;升值;Benguela Current;安哥拉电流; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025579607.html">Role of interannual <fc xmlns="http://www.wiley.com/namespaces/wiley">K</fc>K elvin wave propagations in the equatorial <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A tlantic on the <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A ngola <fc xmlns="http://www.wiley.com/namespaces/wiley">B</fc>B enguela <fc xmlns="http://www.wiley.com/namespaces/wiley">C</fc>C urrent system</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Imbol Koungue Rodrigue Anicet&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Imbol Koungue Rodrigue Anicet,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Illig Serena&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Illig Serena,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rouault Mathieu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rouault Mathieu </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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Role of interannual KK elvin wave propagations in the equatorial AA tlantic on the AA ngola BB enguela CC urrent system

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