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Mixing rates and vertical heat fluxes north of SS valbard from AA rctic winter to spring

机译：北方的混合速率和垂直热量通量 s s 伐木松 a a 森林冬天到春天

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Abstract > Mixing and heat flux rates collected in the Eurasian Basin north of Svalbard during the N‐ICE2015 drift expedition are presented. The observations cover the deep Nansen Basin, the Svalbard continental slope, and the shallow Yermak Plateau from winter to summer. Mean quiescent winter heat flux values in the Nansen Basin are 2 W m ?2 at the ice‐ocean interface, 3 W m ?2 in the pycnocline, and 1 W m ?2 below the pycnocline. Large heat fluxes exceeding 300 W m ?2 are observed in the late spring close to the surface over the Yermak Plateau. The data consisting of 588 microstructure profiles and 50 days of high‐resolution under‐ice turbulence measurements are used to quantify the impact of several forcing factors on turbulent dissipation and heat flux rates. Wind forcing increases turbulent dissipation seven times in the upper 50 m, and doubles heat fluxes at the ice‐ocean interface. The presence of warm Atlantic Water close to the surface increases the temperature gradient in the water column, leading to enhanced heat flux rates within the pycnocline. Steep topography consistently enhances dissipation rates by a factor of four and episodically increases heat flux at depth. It is, however, the combination of storms and shallow Atlantic Water that leads to the highest heat flux rates observed: i ce‐ocean interface heat fluxes average 100 W m ?2 during peak events and are associated with rapid basal sea ice melt, reaching 25 cm/d. </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> > 展示了在N-ICE2015 Drift Expectition的欧亚盆地北部欧亚盆地收集的混合和热量汇率。观察结果覆盖了深度南肯盆地，斯瓦尔巴邦陆地坡，冬季至夏季浅薄的黄金高原。纳森盆地的平均静态冬季热通量值是2 W m ？2 </ sup> 在冰海界面，3个w m ？2 </ sup> 在pycnocline，1 w m ？2 </ sup> 在pycnocline下面。大量的热量超过300 W m ？2 </ sup> 在近春天观察到靠近白金高原的表面。由588微结构型材组成的数据和50天的高分辨率欠冰湍流测量用于量化若干迫使因素对湍流耗散和热通量速率的影响。风迫使在50米上七次增加湍流耗散，并在冰海界面加倍热通量。靠近表面的温暖大西洋水的存在增加了水柱中的温度梯度，导致斑块内的热通量率增强。陡峭地形始终如一地提高耗散率，倍数四个，并在深度上展示了热量的热量。然而，暴风雨和浅大西洋水的组合导致了观察到最高的热通量率： i </ b> CE-OCEAN界面热量平均100 W m ？2 </ sup> 在峰值事件期间，与快速基础海冰熔体相关联，达到25cm / d。 </ 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6期</span><b style="margin: 0 2px;">|</b><span>共18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=Meyer Amelie&option=202" target="_blank" rel="nofollow">Meyer Amelie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fer Ilker&option=202" target="_blank" rel="nofollow">Fer Ilker;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sundfjord Arild&option=202" target="_blank" rel="nofollow">Sundfjord Arild;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peterson Algot K.&option=202" target="_blank" rel="nofollow">Peterson Algot 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>Norwegian Polar Institute Fram CentreTroms? Norway;</p> <p>Geophysical Institute University of Bergen and Bjerknes Centre for Climate ResearchBergen Norway;</p> <p>Norwegian Polar Institute Fram CentreTroms? Norway;</p> <p>Geophysical Institute University of Bergen and Bjerknes Centre for Climate ResearchBergen 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=mixing&option=203" rel="nofollow">mixing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=heat flux&option=203" rel="nofollow">heat flux;</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> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yermak Plateau&option=203" rel="nofollow">Yermak Plateau;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea ice melt&option=203" rel="nofollow">sea ice melt;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Atlantic Water inflow&option=203" rel="nofollow">Atlantic Water inflow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=microstructure profiler&option=203" rel="nofollow">microstructure profiler;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=storms&option=203" rel="nofollow">storms;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=upper ocean&option=203" rel="nofollow">upper ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=N‐ICE2015&option=203" rel="nofollow">N‐ICE2015;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=turbulence&option=203" rel="nofollow">turbulence;</a> </p> <div class="translation"> 机译：混合;热通量;北极;yermak高原;海冰融化;大西洋水流入;微观结构分析器;风暴;上海;N-ICE2015;湍流; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025580262.html">Mixing rates and vertical heat fluxes north of <fc xmlns="http://www.wiley.com/namespaces/wiley">S</fc>S valbard from <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A rctic winter to spring</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meyer Amelie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Meyer Amelie,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fer Ilker&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fer Ilker,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sundfjord Arild&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sundfjord Arild,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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