The Prevalence of Oceanic Surface Modes

LaCasce J. H.

摘要

Abstract >Satellite observations have revolutionized oceanography, capturing diverse phenomena over much of the globe. However, it remains to understand how surface fields, like sea surface height, reflect the motion occurring at depth. The vertical structure of ocean eddies is often expressed in terms of “baroclinic modes,” which are basis functions derived assuming a flat ocean bottom. Bathymetry alters the modes though, weakening the bottom velocities. Using analytical solutions, we demonstrate that with realistic bathymetry and/or bottom friction, the bottom velocities are nearly zero. The resulting “surface modes” should be ubiquitous in the ocean. This would explain the dominant mode of variability obtained from globally distributed current meter data and is consistent with energy spectra derived from sea surface height data. The results yield a simple way to infer subsurface velocities from satellite data and suggest that ocean analyses should be made in terms of surface modes and topographic waves. </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：id =“grl56572-abs-abs-0001”xml：lang =“en”> <title type =“main”>抽象</ title> >卫星观测有革命性的海洋学，捕获多样化在全球范围内的现象。然而，它仍然可以了解表面场，如海面高度，反映深度发生的运动。海洋漩涡的垂直结构通常以“曲金模式”表示，这是假设扁平海底衍生的基函数。沐浴醇虽然改变了模式，削弱了底部速度。使用分析解决方案，我们证明具有现实的浴序和/或底部摩擦，底部速度几乎为零。由此产生的“表面模式”在海洋中应该是普遍的。这将解释从全局分布的电流表数据获得的主导可变性模式，并且与来自海面高度数据的能谱一致。结果产生了一种简单的方法来推断来自卫星数据的地下速度，并表明海洋分析应该在表面模式和地形波方面进行。</ 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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第21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=LaCasce J. H.&option=202" target="_blank" rel="nofollow">LaCasce J. H.;</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 GeosciencesUniversity of OsloOslo Norway;</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=ocean eddies&option=203" rel="nofollow">ocean eddies;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=vertical structure&option=203" rel="nofollow">vertical structure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bathymetry&option=203" rel="nofollow">bathymetry;</a> </p> <div class="translation"> 机译：海洋漩涡;垂直结构;沐浴浴; </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/0704019849507.html">The Prevalence of Oceanic Surface Modes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LaCasce J. H.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">LaCasce J. H. </a> <a href="/journal-foreign-23539/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geophysical Research Letters .</a> <span>2017</span><span>,第21期</span> </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：海洋表面模式的患病率</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070408435583.html">The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shchepetkin AF&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shchepetkin AF,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McWilliams JC&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">McWilliams JC </a> <a href="/journal-foreign-27402/" target="_blank" rel="nofollow" class="tuijian_authcolor">Ocean modelling .</a> <span>2005</span><span>,第4期</span> </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：区域海洋建模系统（ROMS）：明确的，自由表面的，地形跟随坐标的海洋模型</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070408575655.html">Impact on Oceanic Dynamics from Assimilation of Satellite Surface Height Anomaly Data into the Hybrid Coordinate Ocean Model (HYCOM) over the Atlantic Ocean</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tanajura C. 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IGARSS '98. 1998 IEEE International .</a> <span>1998</span> </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：用于被动遥感海洋表面风向的海洋表面泡沫建模</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061515458.html">MODES OF SURFACE CIRCULATION AND CLIMATE OVER THE TROPICAL ATLANTIC, EASTERN PACIFIC, AND INDIAN OCEANS.</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=WOLTER, KLAUS (EDUARD).&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">WOLTER, KLAUS (EDUARD). </a> <span>1987</span> </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：热带大西洋，东太平洋和印度洋的地表环流和气候模式。</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_detail_thesis/040006824995.html">Robust Position Control of an Over-actuated Underwater Vehicle under Model Uncertainties and Ocean Current Effects Using Dynamic Sliding Mode Surface and Optimal Allocation Control</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mai The Vu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mai The Vu,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tat-Hien Le&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tat-Hien Le,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ha Le Nhu Ngoc Thanh&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ha Le Nhu Ngoc Thanh,</a> <span>2021</span> </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：通过动态滑动模式表面和最优分配控制的模型不确定性和海洋电流效应下的过于驱动的水下车辆的鲁棒位置控制</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100022770768.html ">The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content.</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McGregor, Helen V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">McGregor, Helen V.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Evans, Michael N.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Evans, Michael N.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Goosse, Hugues&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Goosse, Hugues,</a> <span>2015</span> </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：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-oceanologica-sinica_thesis/0201253887406.html">全球海洋环流模式中上层海洋对表面强迫的响应和调整Ⅱ.年代际变率</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=容新尧&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 容新尧</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨修群&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨修群</a> <span> <a href="/journal-cn-4977/" 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