The horizontal heat advection in the        <fc xmlns='http://www.wiley.com/namespaces/wiley'>M</fc>M        iddle        <fc xmlns='http://www.wiley.com/namespaces/wiley'>A</fc>A        tlantic        <fc xmlns='http://www.wiley.com/namespaces/wiley'>B</fc>B        ight and the cross‐spectral interactions within the heat advection

Sha Jin; Yan Xiao‐Hai; Li Xiaoming

摘要

Abstract >The upper ocean horizontal heat advection over the middle and outer shelf of the Middle Atlantic Bight (MAB) is investigated using satellite and in situ observations. In the upper mixed layer, the heat advection is mostly positive indicating that it decreases the shelf heat content by bringing cold water from upstream. The domain‐averaged heat advection driven by the barotropic geostrophic current is one‐order larger relative to the density‐driven geostrophic shear and the wind‐driven current. The barotropic geostrophic advection components in the alongshore and offshore direction are of the same order. To investigate the temporal properties of the heat advection, the temperature and currents are decomposed into different time scales using Fast Multidimensional Ensemble Empirical Decomposition (FMEEMD). The cross‐spectral interactions within the advection are quantitatively evaluated with major components identified. Due to the cross‐spectral interaction, energy within the heat advection is found to be redistributed through different time scales, with at least 46.5% variation retained within the original band for the barotropic geostrophic advection. Our results help to better understand the temporal variability of the heat advection, provide a baseline of the nonlinear energy transfer framework within different time scales in the heat advection, and imply the possibility of interplays between short and long‐term oceanic phenomena. </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> >使用卫星和原位观察来研究中大西洋中间架子和外部架子上的上海和外部架子上的上海水平的热平面。在上层混合层中，热平均大多是阳性的，表明它通过从上游的冷水带来冷水来降低储存热含量。由波调性热脑电流驱动的畴平均热平面是相对于密度驱动的地嗜酸性剪切和风驱动电流的单位较大。沿岸和海上方向的波奇脱位性地球化学平流组件是相同的。为了研究热线的时间特性，使用快速多维集合经验分解（FMEEMD），温度和电流分解成不同的时间尺度。通过鉴定的主要组分定量评估平面内的交叉光谱相互作用。由于交叉光谱相互作用，发现热线内的能量被发现通过不同的时间尺度重新分配，至少46.5％的变异在对极性脑筋的原始频段内保留在原始频段内。我们的结果有助于更好地了解热平流的时间变异性，提供了在热线平流中不同时间尺度内的非线性能量转移框架的基线，并意味着短期和长期海洋现象之间相互作用的可能性。</ 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7期</span><b style="margin: 0 2px;">|</b><span>共14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=Sha Jin&option=202" target="_blank" rel="nofollow">Sha Jin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Xiao‐Hai&option=202" target="_blank" rel="nofollow">Yan Xiao‐Hai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Xiaoming&option=202" target="_blank" rel="nofollow">Li Xiaoming;</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>Digital Earth Laboratory Institute of Remote Sensing and Digital Earth Chinese Academy of SciencesBeijing China;</p> <p>College of Earth Ocean and EnvironmentUniversity of DelawareNewark Delaware USA;</p> <p>Digital Earth Laboratory Institute of Remote Sensing and Digital Earth Chinese Academy of SciencesBeijing 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=heat advection&option=203" rel="nofollow">heat advection;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cross‐spectral interaction&option=203" rel="nofollow">cross‐spectral interaction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Middle Atlantic Bight&option=203" rel="nofollow">Middle Atlantic Bight;</a> </p> <div class="translation"> 机译：热进展;跨谱互动;中部大西洋; </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/0704025579733.html">The horizontal heat advection in the <fc xmlns="http://www.wiley.com/namespaces/wiley">M</fc>M iddle <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A tlantic <fc xmlns="http://www.wiley.com/namespaces/wiley">B</fc>B ight and the cross‐spectral interactions within the heat advection</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sha Jin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sha Jin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Xiao‐Hai&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yan Xiao‐Hai,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Xiaoming&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Xiaoming </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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The horizontal heat advection in the MM iddle AA tlantic BB ight and the cross‐spectral interactions within the heat advection

摘要