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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Subseasonal Coastal‐Trapped Wave Propagations in the Southeastern Pacific and Atlantic Oceans: 1. A New Approach to Estimate Wave Amplitude
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Subseasonal Coastal‐Trapped Wave Propagations in the Southeastern Pacific and Atlantic Oceans: 1. A New Approach to Estimate Wave Amplitude

机译：东南太平洋和大西洋的近期沿海捕获波传播：1。一种估算波浪幅度的新方法

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Abstract >The Humboldt and the Benguela upwelling systems are connected to the equatorial variability through the coastal waveguide, so that a large variance of the coastal sea level and current variability can be described as an infinite sum of orthonormal free Coastal‐Trapped Wave (CTW) modes. The objective of this study is to infer the CTW mode contributions to the coastal variability in both systems at subseasonal timescales (<120 days) from regional ocean circulation model simulations. We develop and validate twin regional model configurations of the southeastern Pacific and Atlantic Oceans. Cross‐shore spatial structures of the first four free CTW modes are then derived from model mean stratification and topography along the southwestern African and South American continents. We introduce and validate a new methodology to estimate the gravest CTW mode contributions to model pressure and alongshore current. Our formulation draws on the orthonormality of the CTW modal structures, and uses a simple projection of the coastal and bottom model pressure onto each CTW structure. Results give confidence in the ability of this modal decomposition methodology to disentangle CTW mode contributions from complex nonlinear coastal processes that control the coastal subseasonal variability. In both systems, it allows to successfully extract the gravest poleward propagating CTW modes with velocities close to the theoretical values and amplitudes consistent with the solutions of a simple multimode linear CTW model. Furthermore, results show that both systems exhibit relatively different CTW dynamics and forcings which are discussed in the companion paper (Illig et al., 2018). </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”> <标题类型=“main”>抽象</ title> > Humboldt和Benguela Uppwelling Systems通过沿海波导连接到赤道变异，使沿海的大方差海平和电流可变性可以被描述为无限的正常自由沿海截图波（CTW）模式。本研究的目的是将CTW模式推断到来自区域海洋循环模型模拟的各种时间季度的系统（<120天）的系统中的沿海变异。我们开发和验证东南太平洋和大西洋的双区域模型配置。然后沿着西南部和南美洲大陆的模型平均分层和地形来源于前四种免费CTW模式的交叉岸空间结构。我们介绍并验证新方法，以估算最先进的CTW模式对模型压力和沿岸电流的贡献。我们的配方借鉴了CTW模态结构的正交性，并使用沿海和底部模型压力的简单投影到每个CTW结构上。结果对这种模态分解方法的能力置信到解散来自复杂的非线性沿海过程的CTW模式贡献，这些过程控制沿海暂时的变异性。在两个系统中，它允许成功提取具有靠近理论值的速度和与简单的多模线性CTW模型的解的幅度靠近理论值和幅度的速度来提取敏锐的向外传播CTW模式。此外，结果表明，两种系统表现出相对不同的CTW动态和强制，这些动力学和强制在伴侣论文中讨论（Illig等，2018）。</ 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>2018年第6期</span><b style="margin: 0 2px;">|</b><span>共27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=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=Cadier Emeline&option=202" target="_blank" rel="nofollow">Cadier Emeline;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bachèlery Marie‐Lou&option=202" target="_blank" rel="nofollow">Bachèlery Marie‐Lou;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kersalé Marion&option=202" target="_blank" rel="nofollow">Kersalé Marion;</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>Laboratoire d'Etudes en Géophysique et Océanographie Spatiale (LEGOS) CNRS/IRD/UPS/CNESToulouse France;</p> <p>Department of OceanographyMARE Institute LMI ICEMASA University of Cape TownCape Town South Africa;</p> <p>Department of OceanographyMARE Institute LMI ICEMASA University of Cape TownCape Town South Africa;</p> <p>Department of OceanographyMARE Institute LMI ICEMASA 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=coastal‐trapped waves&option=203" rel="nofollow">coastal‐trapped waves;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=modal decomposition&option=203" rel="nofollow">modal decomposition;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean model simulations&option=203" rel="nofollow">ocean model simulations;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=linear coastal model&option=203" rel="nofollow">linear coastal model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subseasonal variability&option=203" rel="nofollow">subseasonal variability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eastern boundary upwelling systems&option=203" rel="nofollow">eastern boundary upwelling systems;</a> </p> <div class="translation"> 机译：沿海捕获的波浪;模态分解;海洋模型模拟;线性沿海模型;改性变异性;东边界升高系统; </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/0704025580397.html">Subseasonal Coastal‐Trapped Wave Propagations in the Southeastern Pacific and Atlantic Oceans: 1. 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class="tuijian_authcolor"> . 海洋工程 </a> </span> <span> . 1998</span><span>,第1期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-applied-oceanography_thesis/0201254270560.html">西太平洋赤道附近海温与中国东南沿海台风关系的初步分析</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许金镜&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 许金镜</a> <span> <a href="/journal-cn-5020/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 应用海洋学学报 </a> </span> <span> . 1998</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-43375_thesis/020222796716.html">古太平洋早白垩世俯冲作用：来自东南沿海镁铁质侵入岩的岩石地球化学记录</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张博&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张博</a> <a 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href="/patent-detail/06130402288322.html">RADIO WAVE PROPAGATION ESTIMATING APPARATUS, RADIO WAVE PROPAGATION ESTIMATING METHOD, AND RADIO WAVE PROPAGATION ESTIMATING PROGRAM</a> <b>[P]</b> . <span> 外国专利： <!-- 日本专利： --> JP2020036268A </span> <span> . 2020-03-05</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：无线电波传播估计装置，无线电波传播估计方法和无线电波传播估计程序 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704025580397','4',7,2,1,'',this,24)" class="delivery" prompt="010401" 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