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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Nonlinear internal waves and plumes generated in response to sea‐loch outflow, AUVAUV , and time‐lapse photography observations
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Nonlinear internal waves and plumes generated in response to sea‐loch outflow, AUVAUV , and time‐lapse photography observations

机译：非线性内波和响应海路och流出而产生的羽毛， auv auv 和延时摄影观察

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Abstract >The tidally modulated outflow of brackish water from a sea loch forms a thin surface layer that propagates into the coastal ocean as a buoyant gravity current, transporting nutrients and sediments, as well as fresh water, heat and momentum. The fresh intrusion both propagates into and generates a strongly stratified environment which supports trains of nonlinear internal waves (NLIWs). NLIWs are shown to propagate ahead of this buoyancy input in response to propagation of the outflow water into the stratified environment generated by the previous release as well as in the opposing direction after the reflection from steep bathymetry. Oblique aerial photographs were taken and photogrammetric rectification led to the identification of the buoyant intrusion and the subsequent generation of NLIWs. An autonomous underwater vehicle (AUV) was deployed on repeated reciprocal transects in order to make simultaneous CTD, ADCP, and microstructure shear measurements of the evolution of these phenomena in conjunction with conventional mooring measurements. AUV‐based temperature and salinity signals of NLIWs of depression were observed together with increased turbulent kinetic energy dissipation rates of over 2 orders of magnitude within and in the wake of the NLIWs. Repeated measurements allow a unique opportunity to investigate the horizontal structure of these phenomena. Simple metric scaling demonstrates that these processes are likely to be feature of many fjordic systems located on the west coast of Scotland but may also play a key role in the assimilation of the outflow from many tidally dominated fjordic systems throughout the world. </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> >来自海水垫的微咸水的整流流出形成薄的表面层，该薄表面层繁殖到沿海海洋中作为浮力的重力电流，输送营养和沉积物，以及淡水，热量和势头。新鲜的入侵均传播到并产生强烈的环境，该环境支持非线性内部波（NLIWS）的列车。当响应流水的传播进入由先前释放后的分层环境以及从陡峭的沐浴物反射后，响应于之前的释放后的分层环境以及在与陡峭的沐浴物反射之后的相对方向上的分层环境中，NLIW。采用斜空照片，并摄影测量整流导致识别浮力的侵入和随后​​的NLIW。在重复的往复横断面上部署了一种自主水下车辆（AUV），以便与传统的系泊测量结合使用这些现象的演化的同时进行CTD，ADCP和微观结构剪切测量。观察到NLIW的基于AUV的温度和盐度信号，随着湍流动能耗散率的增加，在NLIWS内和在NLIW之后的2个数量级。重复测量允许探讨这些现象的水平结构的独特机会。简单的公制缩放表明，这些过程可能是位于苏格兰西海岸的许多侧影系统的特征，但也可能在遍布全球各地的许多各个峡湾系统的流出中发挥关键作用。</ 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23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=Toberman Matthew&option=202" target="_blank" rel="nofollow">Toberman Matthew;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Inall Mark&option=202" target="_blank" rel="nofollow">Inall Mark;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boyd Tim&option=202" target="_blank" rel="nofollow">Boyd Tim;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dumount Estelle&option=202" target="_blank" rel="nofollow">Dumount Estelle;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Griffiths Colin&option=202" target="_blank" rel="nofollow">Griffiths Colin;</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>Scottish Association for Marine Science Dunstaffnage Marine LaboratoryOban UK;</p> <p>Scottish Association for Marine Science Dunstaffnage Marine LaboratoryOban UK;</p> <p>Scottish Association for Marine Science Dunstaffnage Marine LaboratoryOban UK;</p> <p>Scottish Association for Marine Science Dunstaffnage Marine LaboratoryOban UK;</p> <p>Scottish Association for Marine Science Dunstaffnage Marine LaboratoryOban 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=AUV&option=203" rel="nofollow">AUV;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=buoyant plume&option=203" rel="nofollow">buoyant plume;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=nonlinear internal waves&option=203" rel="nofollow">nonlinear internal waves;</a> </p> <div class="translation"> 机译：AUV;浮力羽毛;非线性内部波; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025579432.html">Nonlinear internal waves and plumes generated in response to sea‐loch outflow, <fc xmlns="http://www.wiley.com/namespaces/wiley">AUV</fc>AUV , and time‐lapse photography observations</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Toberman Matthew&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Toberman Matthew,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Inall Mark&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Inall Mark,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boyd Tim&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Boyd Tim,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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