Coherent Response of Antarctic Intermediate Water and Atlantic Meridional Overturning Circulation During the Last Deglaciation: Reconciling Contrasting Neodymium Isotope Reconstructions From the Tropical Atlantic

Gu Sifan; Liu Zhengyu; Zhang Jiaxu; Rempfer Johannes; Joos Fortunat; Oppo Delia W.

摘要

Abstract > Antarctic Intermediate Water (AAIW) plays important roles in the global climate system and the global ocean nutrient and carbon cycles. However, it is unclear how AAIW responds to global climate changes. In particular, neodymium isotopic composition ( <fi>ε</fi> <sub>Nd</sub> ) reconstructions from different locations from the tropical Atlantic have led to a debate on the relationship between northward penetration of AAIW into the tropical Atlantic and the Atlantic meridional overturning circulation (AMOC) variability during the last deglaciation. We resolve this controversy by studying the transient oceanic evolution during the last deglaciation using a neodymium‐enabled ocean model. Our results suggest a coherent response of AAIW and AMOC: when AMOC weakens, the northward penetration and transport of AAIW decrease while its depth and thickness increase. Our study highlights that as part of the return flow of the North Atlantic Deep Water, the northward penetration of AAIW in the Atlantic is determined predominately by AMOC intensity. Moreover, the inconsistency among different tropical Atlantic <fi>ε</fi> <sub>Nd</sub> reconstructions is reconciled by considering their corresponding core locations and depths, which were influenced by different water masses in the past. The very radiogenic water from the bottom of the Gulf of Mexico and the Caribbean Sea, which was previously overlooked in the interpretations of deglacial <fi>ε</fi> <sub>Nd</sub> variability, can be transported to shallow layers during active AMOC and modulates <fi>ε</fi> <sub>Nd</sub> in the tropical Atlantic. Changes in the AAIW core depth must also be considered. Thus, interpretation of <fi>ε</fi> <sub>Nd</sub> reconstructions from the tropical Atlantic is m </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> >南极中间水（aaiw）在全球气候系统和全球海洋养分中起重要作用和碳循环。但是，尚不清楚Aaiw如何应对全球气候变化。特别地，来自热带大西洋的不同地点的钕同位素组合物（<fi>ε</ fi> <sub> nd </ sub>）重建导致了对北方北方渗透到热带大西洋的关系之间的辩论在最后一个下降期间的大西洋经典推翻循环（AMOC）变异性。我们通过在使用能够钕的海洋模型的最后一个嗜好期间研究瞬态海洋演变来解决这一争议。我们的结果表明AAIW和AMOC的相干响应：当AMOC削弱时，AAIW的向北穿透和运输在其深度和厚度增加时。我们的研究突出显示，作为北大西洋深水回流流量的一部分，大西洋中AAIW的北部渗透是主要通过AMOC强度确定的。此外，通过考虑其相应的核心位置和深度来协调不同热带大西洋<fi> <sub> nd </ sub>重构的不一致。来自墨西哥湾和加勒比海的底部的非常辐射水，之前被忽略在曝光<fi>ε</ fi> <sub> nd </ sub>可变性的解释中，可以运输到浅层在活性Amoc期间并在热带大西洋中调制<fi>ε</ fi> <sub> nd </ sub>。还必须考虑AAIW核心深度的变化。因此，来自热带大西洋的<fi>ε</ fi> <sub> nd </ sub>重建的解释是m </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-28889/'>《Paleoceanography》</a> <b style="margin: 0 2px;">|</b><span>2017年第10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=Gu Sifan&option=202" target="_blank" rel="nofollow">Gu Sifan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Zhengyu&option=202" target="_blank" rel="nofollow">Liu Zhengyu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Jiaxu&option=202" target="_blank" rel="nofollow">Zhang Jiaxu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rempfer Johannes&option=202" target="_blank" rel="nofollow">Rempfer Johannes;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Joos Fortunat&option=202" target="_blank" rel="nofollow">Joos Fortunat;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oppo Delia W.&option=202" target="_blank" rel="nofollow">Oppo Delia W.;</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 Atmospheric and Oceanic Sciences and Center for Climatic ResearchUniversity of Wisconsin‐MadisonMadison WI USA;</p> <p>Department of Atmospheric and Oceanic Sciences and Center for Climatic ResearchUniversity of Wisconsin‐MadisonMadison WI USA;</p> <p>Department of Atmospheric and Oceanic Sciences and Center for Climatic ResearchUniversity of Wisconsin‐MadisonMadison WI USA;</p> <p>Climate and Environmental Physics Physics Institute and Oeschger Center for Climate Change ResearchUniversity of BernBern Switzerland;</p> <p>Now at Computational Physics and Methods and Center for Nonlinear StudiesLos Alamos National LaboratoryLos Alamos NM USA;</p> <p>Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods Hole MA 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/166.html" title="海洋学">海洋学;</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=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=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=deglacial&option=203" rel="nofollow">deglacial;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=neodymium isotope&option=203" rel="nofollow">neodymium isotope;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleocirculation tracer&option=203" rel="nofollow">paleocirculation tracer;</a> </p> <div class="translation"> 机译：aaiw;amoc;延迟;钕同位素;古静电示踪剂; </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 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