Wave Attenuation Through an Arctic Marginal Ice Zone on 12 October 2015: 2. Numerical Modeling of Waves and Associated Ice Breakup

Ardhuin Fabrice; Boutin Guillaume; Stopa Justin; Girard‐Ardhuin Fanny; Melsheimer Christian; Thomson Jim; Kohout Alison; Doble Martin; Wadhams Peter

摘要

Abstract >Many processes that affect ocean surface gravity waves in sea ice give rise to attenuation rates that vary with both wave frequency and amplitude. Here we particularly test the possible effects of basal friction, scattering by ice floes, and dissipation in the ice layer due to dislocations, and ice breakup by the waves. The possible influence of these processes is evaluated in the marginal ice zone of the Beaufort Sea, where extensive wave measurements were performed. The wave data includes in situ measurements and the first kilometer‐scale map of wave heights provided by Sentinel‐1 SAR imagery on 12 October 2015, up to 400 km into the ice. We find that viscous friction at the base of an ice layer gives a dissipation rate that may be too large near the ice edge, where ice is mostly in the form of pancakes. Further into the ice, where larger floes are present, basal friction is not sufficient to account for the observed attenuation. In both regions, the observed narrow directional wave spectra are consistent with a parameterization that gives a weak effect of wave scattering by ice floes. For this particular event, with a dominant wave period around 10 s, we propose that wave attenuation is caused by ice flexure combined with basal friction that is reduced when the ice layer is not continuous. This combination gives realistic wave heights, associated with a 100–200 km wide region over which the ice is broken by waves, as observed in SAR imagery. </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”> <标题类型=“main”>抽象</ title> >影响海冰中海洋表面重力波的许多进程导致衰减率随而有所不同波频和幅度。在这里，我们特别测试基础摩擦，冰浮动的可能影响，并由于位错引起的冰层中的散发，并且波浪的冰块。这些过程的可能影响在Beaufort海的边缘冰区中评估，其中进行了广泛的波测量。波浪数据包括原位测量和由Sentinel-1 SAR Imagery 2015年10月12日提供的波浪高度的第一公里级映射，冰落于400公里。我们发现冰层底部的粘性摩擦给出了冰缘附近可能太大的耗散速率，冰大多是煎饼的形式。进一步进入冰上，其中存在较大的絮状物，基础摩擦力不足以解释观察到的衰减。在两个区域中，观察到的窄定向波谱与参数化一致，该参数化具有通过冰絮凝的波散射的弱效应。对于这种特殊的事件，在大约10秒的主导波期间，我们提出了波衰减是由冰弯曲与基部摩擦结合时引起的，当冰层不连续时减小。这种组合给出了现实的波浪高度，与100-200公里的宽区域相关联，在SAR图像中观察到的冰块被波浪打破。</ 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=Ardhuin Fabrice&option=202" target="_blank" rel="nofollow">Ardhuin Fabrice;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boutin Guillaume&option=202" target="_blank" rel="nofollow">Boutin Guillaume;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stopa Justin&option=202" target="_blank" rel="nofollow">Stopa Justin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Girard‐Ardhuin Fanny&option=202" target="_blank" rel="nofollow">Girard‐Ardhuin Fanny;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Melsheimer Christian&option=202" target="_blank" rel="nofollow">Melsheimer Christian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thomson Jim&option=202" target="_blank" rel="nofollow">Thomson Jim;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kohout Alison&option=202" target="_blank" rel="nofollow">Kohout Alison;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doble Martin&option=202" target="_blank" rel="nofollow">Doble Martin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wadhams Peter&option=202" target="_blank" rel="nofollow">Wadhams Peter;</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>Univ. Brest CNRS IRD Ifremer Laboratoire d'Océanographie Physique et Spatiale IUEMBrest France;</p> <p>Univ. Brest CNRS IRD Ifremer Laboratoire d'Océanographie Physique et Spatiale IUEMBrest France;</p> <p>Univ. Brest CNRS IRD Ifremer Laboratoire d'Océanographie Physique et Spatiale IUEMBrest France;</p> <p>Univ. Brest CNRS IRD Ifremer Laboratoire d'Océanographie Physique et Spatiale IUEMBrest France;</p> <p>Institute of Environmental Physics University of BremenBremen Germany;</p> <p>Applied Physics LaboratoryUniversity of Washington SeattleWashington USA;</p> <p>National Institute of Water and Atmospheric ResearchChristchurch New Zealand;</p> <p>PolarScientific Ltd.Appin UK;</p> <p>Cambridge Polar Consultants Ltd.Cambridge 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=wind‐waves&option=203" rel="nofollow">wind‐waves;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea ice&option=203" rel="nofollow">sea ice;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=WAVEWATCH III&option=203" rel="nofollow">WAVEWATCH III;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SAR&option=203" rel="nofollow">SAR;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Beaufort&option=203" rel="nofollow">Beaufort;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arctic&option=203" rel="nofollow">Arctic;</a> </p> <div class="translation"> 机译：风波;海冰;Wavewatch III;SAR;BEAUFORT;北极; </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> <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/0704025580253.html">Wave Attenuation Through an Arctic Marginal Ice Zone on 12 October 2015: 2. 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