Leads and Associated Sea Ice Drift in the Beaufort Sea in Winter

Lewis Benjiman J.; Hutchings Jennifer K.

摘要

Abstract >Beaufort Sea ice motion is episodic in winter, on average following the anticyclonic motion of the Beaufort Gyre. Weather systems cause the ice pack to fracture in characteristic patterns that depend on the location and trajectory of the weather system in relation to the coast. The majority of leads associated with anticyclonic motion in the Beaufort Sea are coastal leads that form perpendicular from promontories along the coast and landfast ice edge. Between 40% and 90% (depending on location along the Beaufort coast) winter sea ice motion is associated with leads, including coastal leads, coastal flaw leads, and interior lead patterns. In winter much of the Beaufort Gyre ice drift results from ice‐coast interaction, with high ice drift localized on the leeward side of fractures that propagate from the coast. In the vicinity of Point Barrow, which has the largest occurrence of coastal leads, ice drift rates are enhanced due to this ice‐coast interaction. No trends in occurrence of these leads are found over the 20 winters from December 1993 to May 2013. Seasonality in the occurrence of the leads follows seasonality in the location of the Beaufort High. In order for ice to be transported from the northeast part of the Beaufort Gyre to the southwest in a single winter, anticyclones would need to break their geospatial climatic norm, needing a higher prevalence of anticyclones in the eastern Beaufort early in the season and higher prevalence in the west Canada Basin later in the season. </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 =“JGRC23430-Abs-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> > Beaufort海冰运动在冬季，平均后，Beaufort Gyre的反气旋运动。天气系统使冰块以特征模式骨折，这取决于与海岸有关的天气系统的位置和轨迹。与Beaufort海中的反气旋运动相关的大多数领导者是沿海领导，从海岸沿着海岸和陆地冰缘垂直形成垂直。 40％至90％（根据Beaufort海岸的位置，冬季海冰运动与潜在客户有关，包括沿海领导，沿海缺陷领带和室内铅图案。在冬季，冰河互动的大部分嗜好冰漂移导致冰海岸相互作用，高冰漂移，位于从海岸传播的骨折的背风侧。在沿海引线最大的点库附近，由于这种冰海岸相互作用，冰漂移率得到增强。从1993年12月到2013年5月，在20次冬天没有发现这些领导的趋势。在博览会的位置发生的季节性遵循季节性的季节性。为了让冰在一个冬天从博览会的东北部到西南部的冰，反气旋需要打破他们的地理空间气候常态，在本赛季早期需要在东部的东部博览会中患病率较高，普遍存在在西加拿大盆地后盆地盆地。</ 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-34643/'>《Journal of Geophysical Research, C. Oceans: JGR》</a> <b style="margin: 0 2px;">|</b><span>2019年第5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=Lewis Benjiman J.&option=202" target="_blank" rel="nofollow">Lewis Benjiman J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hutchings Jennifer K.&option=202" target="_blank" rel="nofollow">Hutchings Jennifer K.;</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>College of Earth Ocean and Atmospheric SciencesOregon State UniversityCorvallis OR USA;</p> <p>College of Earth Ocean and Atmospheric SciencesOregon State UniversityCorvallis OR USA;</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=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=Beaufort Gyre&option=203" rel="nofollow">Beaufort Gyre;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=kinematics&option=203" rel="nofollow">kinematics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea ice leads&option=203" rel="nofollow">sea ice leads;</a> </p> <div class="translation"> 机译：海冰;Beaufort Gyre;运动学;海冰线; </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/0704025579511.html">Leads and Associated Sea Ice Drift in the Beaufort Sea in Winter</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lewis Benjiman J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lewis Benjiman J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hutchings Jennifer K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hutchings Jennifer K. </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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