Tidal Conversion and Mixing Poleward of the Critical Latitude (an Arctic Case Study)

Rippeth Tom P.; Vlasenko Vasiliy; Stashchuk Nataliya; Scannell Brian D.; Green J. A. Mattias; Lincoln Ben J.; Bacon Sheldon

摘要

Abstract > The tides are a major source of the kinetic energy supporting turbulent mixing in the global oceans. The prime mechanism for the transfer of tidal energy to turbulent mixing results from the interaction between topography and stratified tidal flow, leading to the generation of freely propagating internal waves at the period of the forcing tide. However, poleward of the critical latitude (where the period of the principal tidal constituent exceeds the local inertial period), the action of the Coriolis force precludes the development of freely propagating linear internal tides. Here we focus on a region of sloping topography, poleward of the critical latitude, where there is significant conversion of tidal energy and the flow is supercritical (Froude number, F r 1). A high‐resolution nonlinear modeling study demonstrates the key role of tidally generated lee waves and supercritical flow in the transfer of energy from the barotropic tide to internal waves in these high‐latitude regions. Time series of flow and water column structure from the region of interest show internal waves with characteristics consistent with those predicted by the model, and concurrent microstructure dissipation measurements show significant levels of mixing associated with these internal waves. The results suggest that tidally generated lee waves are a key mechanism for the transfer of energy from the tide to turbulence poleward of the critical latitude. </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 =“Grl56750-Abs-abs-0001”> <标题类型=“main”>抽象</ title> >潮汐是一个主要来源支持在全球海洋中湍流混合的动能。潮汐能转移到湍流混合结果的主要机制来自地形和分层潮流之间的相互作用，导致在强制潮汐期间自由传播内部波。然而，临界纬度的极端（主要潮汐成分超出局部惯性时期的情况），科里奥利力的作用绝不能释放自由繁殖的线性内部潮汐的发展。在这里，我们专注于倾斜地形的区域，临界纬度的极端，其中潮汐能的显着转化，流量是超临界的（Froude号， f </ i> R </ i>＆gt ; 1）。高分辨率非线性建模研究证明，在这些高纬度地区的压力学潮中将能量转移到能量转移到内部波的关键作用。来自感兴趣区域的流量和水柱结构的时间序列显示具有与模型预测的特性的内部波，并发的微观结构耗散测量结果显示出与这些内部波相关的显着水平。结果表明，整个产生的Lee波是从潮汐到临界纬度的湍流的能量的关键机制。 </ 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9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=Rippeth Tom P.&option=202" target="_blank" rel="nofollow">Rippeth Tom P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vlasenko Vasiliy&option=202" target="_blank" rel="nofollow">Vlasenko Vasiliy;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stashchuk Nataliya&option=202" target="_blank" rel="nofollow">Stashchuk Nataliya;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Scannell Brian D.&option=202" target="_blank" rel="nofollow">Scannell Brian D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Green J. A. Mattias&option=202" target="_blank" rel="nofollow">Green J. A. Mattias;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lincoln Ben J.&option=202" target="_blank" rel="nofollow">Lincoln Ben J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bacon Sheldon&option=202" target="_blank" rel="nofollow">Bacon Sheldon;</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>School of Ocean SciencesBangor UniversityBangor UK;</p> <p>School of Biological and Marine SciencesPlymouth UniversityPlymouth UK;</p> <p>School of Biological and Marine SciencesPlymouth UniversityPlymouth UK;</p> <p>School of Ocean SciencesBangor UniversityBangor UK;</p> <p>School of Ocean SciencesBangor UniversityBangor UK;</p> <p>School of Ocean SciencesBangor UniversityBangor UK;</p> <p>National Oceanography CentreSouthampton UK;</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=turbulence&option=203" rel="nofollow">turbulence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mixing&option=203" rel="nofollow">mixing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tide&option=203" rel="nofollow">tide;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arctic Ocean&option=203" rel="nofollow">Arctic Ocean;</a> </p> <div class="translation"> 机译：湍流;混合;潮;北冰洋; 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2019</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061204036822.html">沉砂式近岸潮汐能转换装置及其潮汐能和波能的转换方法</a> <b>[P]</b> . <span> 中国专利： CN109611262B </span> <span> . 2020.10.09</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120100516575.html">沉砂式近岸潮汐能转换装置及其潮汐能和波能的转换方法</a> <b>[P]</b> . <span> 中国专利： CN109611262A </span> <span> . 2019-04-12</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130420233205.html">ROTARY-TYPE WIND TURBINE FOR ARCTIC LATITUDES</a> <b>[P]</b> . <span> 外国专利：  UA100785C2 </span> <span> . 2013-01-25</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：北极纬向的旋转式风轮机 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130500183840.html">FUNCTIONAL PRODUCT OF MIXED COMPOSITION, INCLUDING PLANT AND ANIMAL COMPONENTS OF NORTHERN LATITUDES</a> <b>[P]</b> . <span> 外国专利：  RU2750217C1 </span> <span> . 2021-06-24</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：混合组成的功能产物，包括北纬植物和动物组分 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130430703240.html">Low-Cost, Mass-Producible Container for Separately Storing at Least Two Substances of Any Ratio for Subsequent Mixing, a.k.a., "TIDAL TWIST" and "TIDAL FORCE"</a> <b>[P]</b> . <span> 外国专利：  US2008314775A1 </span> <span> . 2008-12-25</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：低成本，可大量生产的容器，可以至少以任意比例分别存放两种物质进行后续混合，也称为“ TIDAL TWIST”和“ TIDAL FORCE” </span> </p> </li> </ul> </div> </div> </div> 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