Observational Inferences of Lateral Eddy Diffusivity in the Halocline of the Beaufort Gyre

Meneghello Gianluca; Marshall John; Cole Sylvia T.; Timmermans Mary‐Louise

摘要

Abstract > Using Ekman pumping rates mediated by sea ice in the Arctic Ocean's Beaufort Gyre (BG), the magnitude of lateral eddy diffusivities required to balance downward pumping is inferred. In this limit—that of vanishing residual‐mean circulation—eddy‐induced upwelling exactly balances downward pumping. The implied eddy diffusivity varies spatially and decays with depth, with values of 50–400?m 2 /s. Eddy diffusivity estimated using mixing length theory applied to BG mooring data exhibits a similar decay with depth and range of values from 100?m 2 /s to more than 600?m 2 /s. We conclude that eddy diffusivities in the BG are likely large enough to balance downward Ekman pumping, arresting the deepening of the gyre and suggesting that eddies play a zero‐order role in buoyancy and freshwater budgets of the BG. </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 =“Grl56718-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> >使用海冰介导的Ekman抽水率在北冰洋的博彩景观（BG）中，推断出平衡向下泵送所需的横向涡流的大小。在这种限制 - 消失的残余平均循环 - 涡流诱导的升高的较余平衡向下泵送。隐含的涡流扩散率在空间上变化并衰减深度，值为50-400Ωm 2 </ sup> / s。使用应用于BG系泊数据的混合长度理论估计的涡流扩散率呈现与100μm 2 2 </ sup> 2 </ sup> 2 </ sup> 2 </ sup> 2 </ sup> 2 </ sup> 2 </ sup> 2 </ sup> 2 </ sup> 2 / s。我们得出结论，BG中的涡流扩散可能足够大，以平衡向下的EKMAN抽水，逮捕陀螺仪的深化，并提出漩涡在BG的浮力和淡水预算中发挥零级角色。 </ p> </ abstract> </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>2017年第24期</span><b style="margin: 0 2px;">|</b><span>共8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=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=Cole Sylvia T.&option=202" target="_blank" rel="nofollow">Cole Sylvia T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Timmermans Mary‐Louise&option=202" target="_blank" rel="nofollow">Timmermans Mary‐Louise;</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 Earth Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>Department of Earth Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridge MA USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Department of Geology and GeophysicsYale UniversityNew Haven CT USA;</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=eddy diffusivity&option=203" rel="nofollow">eddy diffusivity;</a> <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=observation&option=203" rel="nofollow">observation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=freshwater budget&option=203" rel="nofollow">freshwater budget;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ekman pumping&option=203" rel="nofollow">Ekman pumping;</a> </p> <div class="translation"> 机译：涡流扩散;Beaufort Gyre;观察;淡水预算;ekman泵送; 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