首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >A Three‐Way Balance in the Beaufort Gyre: The Ice‐Ocean Governor, Wind Stress, and Eddy Diffusivity
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A Three‐Way Balance in the Beaufort Gyre: The Ice‐Ocean Governor, Wind Stress, and Eddy Diffusivity

机译:Beaufort Gyre中的三方平衡:冰海洋调速器,风力应力和涡流扩散率

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摘要

Abstract >The Beaufort Gyre (BG) is a large anticyclonic circulation in the Arctic Ocean. Its strength is directly related to the halocline depth, and therefore also to the storage of freshwater. It has recently been proposed that the equilibrium state of the BG is set by the Ice‐Ocean Governor, a negative feedback between surface currents and ice‐ocean stress, rather than a balance between lateral mesoscale eddy fluxes and surface Ekman pumping. However, mesoscale eddies are present in the Arctic Ocean; it is therefore important to extend the Ice‐Ocean Governor theory to include lateral fluxes due to mesoscale eddies. Here, a nonlinear ordinary differential equation is derived that represents the effects of wind stress, the Ice‐Ocean Governor, and eddy fluxes. Equilibrium and time‐varying solutions to this three‐way balance equation are obtained and shown to closely match the output from a hierarchy of numerical simulations, indicating that the analytical model represents the processes controlling BG equilibration. The equilibration timescale derived from this three‐way balance is faster than the eddy equilibration timescale and slower than the Ice‐Ocean Governor equilibration timescales for most values of eddy diffusivity. The sensitivity of the BG equilibrium depth to changes in eddy diffusivity and the presence of the Ice‐Ocean Governor is also explored. These results show that predicting the response of the BG to changing surface forcing and sea ice conditions requires faithfully capturing the three‐way balance between the Ice‐Ocean Governor, wind stress, and eddy fluxes. </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”XML:ID =“JGRC23404-Abs-Abs-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> > beaufort gyre(bg)是一个北冰洋大的反气旋循环。其强度与卤划线深度直接相关,因此也可以储存淡水。最近提出,BG的均衡状态由冰海洋调速器设置,表面电流和冰海洋压力之间的负反馈,而不是横向Mescle涡流和表面Ekman泵之间的平衡。然而,Mesoscale Eddies存在于北冰洋中;因此,延伸冰海洋调速器理论以包括由于Messcale Eddies而延伸的横向助焊剂。这里,推导出非线性常微分方程,其代表风力应力,冰海洋调速器和涡流的影响。获得对该三方平衡方程的平衡和时变解,并显示与数值模拟的层次结构密切匹配,表明分析模型代表控制BG平衡的过程。从这种三方平衡导出的平衡时间尺度比涡流速度速度快,比冰波调速器平衡时间慢,以获得大多数涡流扩散率的值。还探讨了BG平衡深度对涡流扩散率变化的敏感性以及冰海州州长的存在。这些结果表明,预测BG对变化表面迫使和海冰条件的响应需要忠实地捕捉冰海调速器,风力应力和涡流之间的三方平衡。</ 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>2019年第5期</span><b style="margin: 0 2px;">|</b><span>共18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=Doddridge Edward W.&option=202" target="_blank" rel="nofollow">Doddridge Edward W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meneghello Gianluca&option=202" target="_blank" rel="nofollow">Meneghello Gianluca;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marshall John&option=202" target="_blank" rel="nofollow">Marshall John;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Scott Jeffery&option=202" target="_blank" rel="nofollow">Scott Jeffery;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lique Camille&option=202" target="_blank" rel="nofollow">Lique Camille;</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>Earth Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>Earth Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>Earth Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>Earth Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>Laboratoire d'Océanographie Physique et Spatiale Université de Bretagne Occidentale CNRS IRD Ifremer IUEMBrest France;</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=Beaufort Gyre&option=203" rel="nofollow">Beaufort Gyre;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ice‐Ocean Governor&option=203" rel="nofollow">Ice‐Ocean Governor;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mesoscale eddies&option=203" rel="nofollow">mesoscale eddies;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arctic&option=203" rel="nofollow">Arctic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea ice&option=203" rel="nofollow">sea ice;</a> </p> <div class="translation"> 机译:Beaufort Gyre;冰海州州长;Mesoscale Eddies;北极;海冰; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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/0704025580498.html">A Three‐Way Balance in the Beaufort Gyre: The Ice‐Ocean Governor, Wind Stress, and Eddy Diffusivity</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doddridge Edward W.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Doddridge Edward W.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meneghello Gianluca&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Meneghello Gianluca,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marshall John&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Marshall John,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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<a href="/conference-cn-40447/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第六届广西青年学术年会 </a> <span> <span> . 2013</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020313743056.html">热带气旋在海洋能量平衡和水团平衡中的作用</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘玲玲&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘玲玲</a> <span> . 2008</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061203716924.html">一种基于液压随动系统静态平衡的调速器比例阀中位调整方法</a> <b>[P]</b> . <span> 中国专利: CN108468616B </span> <span> . 2020.04.24</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120110963767.html">一种基于液压随动系统静态平衡的调速器比例阀中位调整方法</a> <b>[P]</b> . <span> 中国专利: CN108468616A </span> <span> . 2018-08-31</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130428762047.html">Oceanic model steady state decision manner, the wind stress data of the oceanic model steady state</a> <b>[P]</b> . <span> 外国专利: <!-- 日本专利: --> JP4525163B2 </span> <span> . 2010-08-18</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:海洋模型稳态决策方式,海洋模型稳态风应力数据 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130427015966.html">FLOATING ON THE OCEAN WIND POWER GENERATOR SYSTEM OF ACCORDING NACELLE AUTOMATICALLY ADJUST THE BALANCE OF THE WIND DEVICE</a> <b>[P]</b> . <span> 外国专利: <!-- 韩国专利: --> KR20100077903A </span> <span> . 2010-07-08</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:漂浮在按照纳赛尔自动调节风量平衡的海洋风发电机系统上 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130429264406.html">Arrangement for converting wind energy over open water, especially ocean, into electrical energy has free-flow water turbine(s) or diffuser or vortex flow turbines driven by wind, towed or tethered sail(s) and/or by Flettner rotor(s)</a> <b>[P]</b> . <span> 外国专利: <!-- 德国专利: --> DE102007057267A1 </span> <span> . 2008-11-27</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:用于将开放水域(特别是海洋)上的风能转换为电能的装置具有自由流动的水轮机或扩散器或涡流涡轮机,这些水轮机由风,拖曳或束缚的风帆和/或由弗莱特纳转子驱动 </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;" > 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