Drivers of Interannual Variability of Summer Mixed Layer Depth in the Southern Ocean Between 2002 and 2011

机译：2002年至2011年南海夏季混合层深度持续变异的驱动因素

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Abstract >Climate change projections indicate that there will be warming and an intensification of westerly winds in the Southern Ocean (SO) in the future. These two forcings potentially have opposing effects on the depth of the surface mixed layer. Here we investigate how interannual to decadal variability of atmospheric surface air temperature (SAT) and zonal wind speed (uwind) impact mixed layer depth (MLD) in the SO (south of 30°S) during summer, the season of main biological activity. We use gridded MLD data from observations and atmospheric reanalysis data of uwind and SAT in the SO to assess summer MLD variability and its potential drivers. With a model‐based sensitivity experiment, we quantify the relative contributions of uwind versus SAT forcing on the summer MLD in the decade 2002–2011. Wind‐induced changes dominate over temperature‐induced changes of the MLD between 2002 and 2011. We find a positive trend of summer MLD in the Antarctic Zone of the Atlantic and Indian Ocean sectors. Our model‐based sensitivity study suggests that the summer MLD shows a zonally asymmetric response to recent atmospheric forcing. In the Pacific and Australian sectors, cooling and intensification of uwind jointly result in a deepening of the mixed layer. In the Atlantic and Indian sectors, the MLD responds differently north and south of the Antarctic Polar Front (APF). A deepening south of the APF is caused by the increase in uwind, whereas the decrease in uwind and warming act in concert to result in a shoaling of the MLD north of the APF. </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 =“JGRC23016-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> >气候变化投影表明会有未来南海（SO）在南海（SO）的温暖和强化加剧。这两个强制可能对表面混合层的深度具有相反的影响。在这里，我们研究了大气表面空气温度（SAT）和Zonal风速（UWind）的季节（在30°S南部）的季节，主要生物活性季节的互动变异性（SAT）和带状风速（UWIND）冲击混合层深度（MLD）。我们使用来自UWIND的观测和大气再分析数据的网格MLD数据，并坐在那里，以评估夏季MLD可变性及其潜在司机。通过基于模型的敏感性实验，我们在2002-2011十年中量化了uwind对夏季MLD的相对贡献。风力诱导的变化在2002年和2011年间的温度诱导的MLD变化中占据主导地位。我们在大西洋和印度洋部门的南极区发现了夏季MLD的积极趋势。我们基于模型的敏感性研究表明，夏季MLD对最近的大气强制表现出对阵不对称的反应。在太平洋和澳大利亚部门，卷畅的冷却和强化共同导致混合层的深化。在大西洋和印度部门，MLD在南极极性前沿（APF）的北方和南方不同地回应。 APF的南部深化是由uwind的增加引起的，而uwind和变暖行为的减少，以导致APF的北部的MLD浅。</ 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>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共14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=Panassa E.&option=202" target="_blank" rel="nofollow">Panassa E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=V?lker C.&option=202" target="_blank" rel="nofollow">V?lker C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wolf‐Gladrow D.&option=202" target="_blank" rel="nofollow">Wolf‐Gladrow D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hauck J.&option=202" target="_blank" rel="nofollow">Hauck 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>Alfred‐Wegener-Institut Helmholtz Zentrum für Polar‐ und Meeresforschung (AWI)Bremerhaven Germany;</p> <p>Alfred‐Wegener-Institut Helmholtz Zentrum für Polar‐ und Meeresforschung (AWI)Bremerhaven Germany;</p> <p>Alfred‐Wegener-Institut Helmholtz Zentrum für Polar‐ und Meeresforschung (AWI)Bremerhaven Germany;</p> <p>Alfred‐Wegener-Institut Helmholtz Zentrum für Polar‐ und Meeresforschung (AWI)Bremerhaven Germany;</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;"> </p> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:22:17</span> </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/0704025579369.html">Drivers of Interannual Variability of Summer Mixed Layer Depth in the Southern Ocean Between 2002 and 2011</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Panassa E.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Panassa E.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=V?lker C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">V?lker C.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wolf‐Gladrow D.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wolf‐Gladrow D.,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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