Submesoscale processes promote seasonal restratification in the        <fc xmlns='http://www.wiley.com/namespaces/wiley'>S</fc>S        ubantarctic        <fc xmlns='http://www.wiley.com/namespaces/wiley'>O</fc>O        cean

du Plessis M.; Swart S.; Ansorge I. J.; Mahadevan A.

摘要

Abstract >Traditionally, the mechanism driving the seasonal restratification of the Southern Ocean mixed layer (ML) is thought to be the onset of springtime warming. Recent developments in numerical modeling and North Atlantic observations have shown that submesoscale ML eddies (MLE) can drive a restratifying flux to shoal the deep winter ML prior to solar heating at high latitudes. The impact of submesoscale processes on the intraseasonal variability of the Subantarctic ML is still relatively unknown. We compare 5 months of glider data in the Subantarctic Zone to simulations of a 1‐D mixing model to show that the magnitude of restratification of the ML cannot be explained by heat, freshwater, and momentum fluxes alone. During early spring, we estimate that periodic increases in the vertical buoyancy flux by MLEs caused small increases in stratification, despite predominantly down‐front winds that promote the destruction of stratification. The timing of seasonal restratification was consistent between 1‐D model estimates and the observations. However, during up‐front winds, the strength of springtime stratification increased over twofold compared to the 1‐D model, with a rapid shoaling of the MLD from 200 m to 100 m within a few days. The ML stratification is further modified under a negative Ekman buoyancy flux during down‐front winds, resulting in the destruction of ML stratification and deepening of the MLD. These results propose the importance of submesoscale buoyancy fluxes enhancing seasonal restratification and mixing of the Subantarctic ML. </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> >传统上，驾驶季节性抑制南海混合层（ML）的机构被认为是春天变暖的发作。最近在数值建模和北大西洋观测中的发展已经表明，亚透明度ML EDDIES（MLE）可以在高纬度地区的太阳能加热之前驱动瑞克服深度冬季ML。提子尺度过程对小提治局ML的初始变异性的影响仍然是相对未知的。我们将5个月的Prophidic区的滑翔机数据进行比较至1-D混合模型的模拟，以表明ML的restafation的幅度不能通过热，淡水和动量通量来解释。在早春期间，我们估计MLES由MLES垂直浮力通量的周期性增加引起的分层增加，尽管主要是促进分层破坏的颠簸。季节性克制的时间在1-D模型估计和观察结果之间是一致的。然而，在上部风中，与1-D型号相比，春天分层的强度增加了两倍，并且在几天内从＆ 200米到100米的快速俯就。在下线风中的负ekman浮力通量下进一步修改M1分层，导致ML分层和MLD加深的破坏。这些结果提出了提高核心浮力通量增强季节性抑制和细胞抑制混合的重要性。</ 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4期</span><b style="margin: 0 2px;">|</b><span>共16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=du Plessis M.&option=202" target="_blank" rel="nofollow">du Plessis M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Swart S.&option=202" target="_blank" rel="nofollow">Swart S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ansorge I. J.&option=202" target="_blank" rel="nofollow">Ansorge I. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mahadevan A.&option=202" target="_blank" rel="nofollow">Mahadevan A.;</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 OceanographyMarine Research Institute University of Cape TownRondebosch South Africa;</p> <p>Department of OceanographyMarine Research Institute University of Cape TownRondebosch South Africa;</p> <p>Department of OceanographyMarine Research Institute University of Cape TownRondebosch South Africa;</p> <p>Physical Oceanography DepartmentWoods Hole Oceanographic InstitutionWoods Hole Massachusetts 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=ocean gliders&option=203" rel="nofollow">ocean gliders;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Southern Ocean&option=203" rel="nofollow">Southern Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seasonal stratification&option=203" rel="nofollow">seasonal stratification;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=1‐D mixed‐layer model&option=203" rel="nofollow">1‐D mixed‐layer model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mixed layer eddies&option=203" rel="nofollow">mixed layer eddies;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ekman buoyancy flux&option=203" rel="nofollow">Ekman buoyancy flux;</a> </p> <div class="translation"> 机译：海洋滑翔机;南洋;季节性分层;1-D混合层模型;混合层漩涡;ekman浮力通量; </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/0704025579442.html">Submesoscale processes promote seasonal restratification in the <fc xmlns="http://www.wiley.com/namespaces/wiley">S</fc>S ubantarctic <fc xmlns="http://www.wiley.com/namespaces/wiley">O</fc>O cean</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=du Plessis M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">du Plessis M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Swart S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Swart S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ansorge I. 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Submesoscale processes promote seasonal restratification in the SS ubantarctic OO cean

摘要