Decoupled Freshwater Transport and Meridional Overturning in the South Atlantic

Mignac D.; Ferreira D.; Haines K.

摘要

Abstract > Freshwater transports type="mathematics"> ( F <sub> ov </sub> ) by the Atlantic meridional overturning circulation (AMOC) are sensitive to salinity distributions and may determine AMOC stability. However, climate models show large salinity biases, distorting the relation between type="mathematics"> F <sub> ov </sub> and the AMOC. Using free‐running models and ocean reanalyses with realistic salinities but quite different AMOCs, we show that the fresh Antarctic Intermediate Water layer eliminates salinity differences across the AMOC branches at ~1,200?m, ? type="mathematics"> S <sub> 1200 m </sub> , which decouples type="mathematics"> F <sub> ov </sub> from the AMOC south of ~10°N. As the Antarctic Intermediate Water disappears north of ~10°N, a large ? type="mathematics"> S <sub> 1200 m </sub> allows the AMOC to drive substantial southward type="mathematics"> F <sub> ov </sub> in the North Atlantic. In the South Atlantic the 0–300 m zonal salinity contrasts control the gyre freshwater transports type="mathematics"> F <sub> gyre </sub> , which also determine the total freshwater transports. This decoupling makes the southern </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> >淡水传输 type =“数学”>（ f </ i> <Sub> </ s ov </ sup> </ span>）由大西洋化学倾覆循环（Amoc）对盐度分布敏感，并且可以确定Amoc稳定性。然而，气候模型显示出大的盐度偏差，扭曲<跨度类型=“数学”之间的关系> f </ i> <sub> ov </ sup> </ span>和amoc。使用自由运行的模型和海洋Reanalyses具有现实盐度但是amocs的完美盐度，我们表明新鲜的南极中间水层消除了〜1,200？m的武器分支中的盐度差异，？ type =“数学”> s </ i> <sub> 1200 m </ sum> </ sub> </ span>，哪个decouples type =“momatematics”> f <sub> </ i> </ sup> </ span>从〜10°N的amoc南部。由于南极中间水在左右消失〜10°N，一个大？ type =“数学”> s </ i> <sub> 1200 m </ i> </ sub> </ span>允许amoc驱动大量南方 type =“momatematics” > f </ i> <sub> 北大西洋中的 ov </ sub> </ span> </ sub> </ span>。在南部大西洋中，0-300米Zonal盐度对比控制淡水淡水输送<跨度=“数学”> F </ i> <sub> gyre </ i> </ sub> </ SPAN>，其还确定了总淡水输送。这种去耦使南部 </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共9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=Mignac D.&option=202" target="_blank" rel="nofollow">Mignac D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferreira D.&option=202" target="_blank" rel="nofollow">Ferreira D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haines K.&option=202" target="_blank" rel="nofollow">Haines 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>Department of MeteorologyUniversity of ReadingReading UK;</p> <p>Department of MeteorologyUniversity of ReadingReading UK;</p> <p>Department of Meteorology and National Centre for Earth ObservationUniversity of ReadingReading 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=AMOC&option=203" rel="nofollow">AMOC;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=overturning&option=203" rel="nofollow">overturning;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=gyre&option=203" rel="nofollow">gyre;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=AAIW&option=203" rel="nofollow">AAIW;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean reanalyses&option=203" rel="nofollow">ocean reanalyses;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bistability&option=203" rel="nofollow">bistability;</a> </p> <div class="translation"> 机译：amoc;翻转;圆形;aaiw;海洋Reanalyses;双稳态; </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/0704019852389.html">Decoupled Freshwater Transport and Meridional Overturning in the South Atlantic</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mignac D.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mignac D.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferreira D.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ferreira D.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haines K.&option=202" target="_blank" rel="nofollow" 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