The Influence of Tide and Wind on the Propagation of Fronts in a Shallow River Plume

Rijnsburger Sabine; Flores Raúl P.; Pietrzak Julie D.; Horner‐Devine Alexander R.; Souza Alejandro J.

摘要

Abstract >In this study we used field data and radar images to investigate the influence of winds and tides on the propagation of tidal plume fronts. The measurements were collected in a shallow shelf region off the Dutch coast, 10?km north of the Rhine River mouth, and they clearly show the passage of distinct freshwater lenses and associated fronts at the surface that propagate all the way to the coastline. These fronts are observed as a sudden drop in near‐surface salinity, accompanied by high cross‐shore shear with onshore velocities at the surface. We determined the arrival time to our measurement site, frontal propagation speed, and structure of the fronts by combining the in situ data and radar images. Frontal Froude numbers show a wide range of values, with an average of 0.44. Our results show that fronts during spring tides are thinner, more mixed, and move faster relative to the ground during calm spring tides when compared to calm neap tides. Downwelling winds during spring tides result in thicker and faster fronts; however, the intrinsic frontal propagation speed indicates that the wind and tide control the frontal propagation mainly due to advection rather than by changing the frontal structure. Strong return currents in the near‐bed layer resulting from fast and thick fronts increase near‐bed turbulence and bed stresses. These high stresses suggest that the passage of fronts in shallow coastal areas can initiate sediment resuspension and contribute to transport processes. </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 =“JGRC22981-ABS-ABS-ABS-0001”> <Title Type =“Main”> Abstract </ Title> >在本研究中我们使用了现场数据和雷达图像探讨风和潮汐对潮汐羽流量传播的影响。测量在荷兰海岸的浅货架区中收集，莱茵河嘴北沿北部10克，并清楚地显示了不同的淡水透镜和相关前锋在沿着海岸线传播的表面的通道。这些前线被观察到近表面盐度突然下降，伴随着高度的横岸剪切，在表面处具有陆上速度。我们通过组合原位数据和雷达图像确定到达我们的测量站点，正面传播速度和面部的结构的到达时间。 Frontal Froude号码显示出广泛的值，平均为0.44。我们的结果表明，与平静的NeAP潮汐相比，春季潮汐期间的前线更加混合，更加混合，并在平静的弹簧潮汐期间相对于地面移动更快。春季潮汐期间的沉船导致较厚且较快的前线;然而，内在的额头传播速度表明风和潮汐控制正面传播主要是由于前进而不是通过改变正面结构。近床层中的强返回电流由快速和厚的前部增加近床湍流和床胁迫。这些高应力表明，浅沿海地区的前沿通过沉积物重新悬浮，并有助于运输过程。</ 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>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共17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=Rijnsburger Sabine&option=202" target="_blank" rel="nofollow">Rijnsburger Sabine;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Flores Raúl P.&option=202" target="_blank" rel="nofollow">Flores Raúl P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pietrzak Julie D.&option=202" target="_blank" rel="nofollow">Pietrzak Julie D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Horner‐Devine Alexander R.&option=202" target="_blank" rel="nofollow">Horner‐Devine Alexander R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Souza Alejandro J.&option=202" target="_blank" rel="nofollow">Souza Alejandro J.;</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 Hydraulic EngineeringDelft University of TechnologyDelft Netherlands;</p> <p>Department of Civil and Environmental EngineeringUniversity of WashingtonSeattle WA USA;</p> <p>Department of Hydraulic EngineeringDelft University of TechnologyDelft Netherlands;</p> <p>Department of Civil and Environmental EngineeringUniversity of WashingtonSeattle WA USA;</p> <p>CINVESTAVMérida Mexico;</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=plume fronts&option=203" rel="nofollow">plume fronts;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=density stratification&option=203" rel="nofollow">density stratification;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=in situ data&option=203" rel="nofollow">in situ data;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reynolds stresses&option=203" rel="nofollow">Reynolds stresses;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=river plume&option=203" rel="nofollow">river plume;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ROFI&option=203" rel="nofollow">ROFI;</a> </p> <div class="translation"> 机译：羽毛锋利;密度分层;原位数据;雷诺强调;河流;rofi; </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/0704025580202.html">The Influence of Tide and Wind on the Propagation of Fronts in a Shallow River Plume</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rijnsburger Sabine&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rijnsburger Sabine,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Flores Raúl P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Flores Raúl P.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pietrzak Julie D.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pietrzak Julie D.,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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href="/patent-detail/06130496214209.html">Sensing force generator in place of the force of the current of rivers, rivers, tides, etc.</a> <b>[P]</b> . <span> 外国专利：  FR631180A </span> <span> . 1927-12-15</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：感应力发生器代替河流，河流，潮汐等的潮流 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130427106132.html">Environmentally friendly process for purifying build a bottom emission type device, the reservoir on the river or river front end width by contaminated river water by using a gravity method to discharge the first heavy shingles on a clean river bottoms so that the river water is clean.</a> <b>[P]</b> . <span> 外国专利：  KR20090130165A </span> <span> . 2009-12-18</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: 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