The Spatial Structure of the 128?ka Antarctic Sea Ice Minimum

Holloway Max D.; Sime Louise C.; Allen Claire S.; Hillenbrand Claus‐Dieter; Bunch Pete; Wolff Eric; Valdes Paul J.

摘要

Abstract > We compare multi‐ice core data with δ 18 O model output for the early last interglacial Antarctic sea ice minimum. The spatial pattern of δ 18 O across Antarctica is sensitive to the spatial pattern of sea ice retreat. Local sea ice retreat increases the proportion of winter precipitation, depleting δ 18 O at ice core sites. However, retreat also enriches δ 18 O because of the reduced source‐to‐site distance for atmospheric vapor. The joint overall effect is for δ 18 O to increase as sea ice is reduced. Our data‐model comparison indicates a winter sea ice retreat of 67, 59, and 43% relative to preindustrial in the Atlantic, Indian, and Pacific sectors of the Southern Ocean. A compilation of Southern Ocean sea ice proxy data provides weak support for this reconstruction. However, most published marine core sites are located too far north of the 128,000?years B.P. sea ice edge, preventing independent corroboration for this sea ice reconstruction. </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：ID =“Grl56570-Abs-Abs-0001”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >我们比较多冰核心数据δ</ i> 18 </ sup> o模型输出，用于早期的上间南极海冰最小。南极洲横跨南极的δ</ i> 18 </ sup> o的空间模式对海冰撤退的空间模式敏感。当地海冰撤退增加了冬季沉淀的比例，在冰芯部位处耗尽δ</ i> 18℃。然而，由于对大气蒸汽的源极距离降低，还始于富集δ</ i> 18 </ sup> o。随着海冰减少，接合总效应对于δ</ i> 18 </ sup> o增加。我们的数据型号比较表明，相对于南海大西洋，印度和太平洋地区的预工业，67,59和43％的冬季海冰。南洋海冰代理数据的汇编为这一重建提供了薄弱的支持。然而，大多数公布的海洋核心网站位于128,000年以北的距离太远？多年B.P.海冰缘，防止独立的碳化为这片海冰重建。 </ 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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第21期</span><b style="margin: 0 2px;">|</b><span>共11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=Holloway Max D.&option=202" target="_blank" rel="nofollow">Holloway Max D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sime Louise C.&option=202" target="_blank" rel="nofollow">Sime Louise C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Allen Claire S.&option=202" target="_blank" rel="nofollow">Allen Claire S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hillenbrand Claus‐Dieter&option=202" target="_blank" rel="nofollow">Hillenbrand Claus‐Dieter;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bunch Pete&option=202" target="_blank" rel="nofollow">Bunch Pete;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wolff Eric&option=202" target="_blank" rel="nofollow">Wolff Eric;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Valdes Paul J.&option=202" target="_blank" rel="nofollow">Valdes Paul 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>British Antarctic SurveyCambridge UK;</p> <p>British Antarctic SurveyCambridge UK;</p> <p>British Antarctic SurveyCambridge UK;</p> <p>British Antarctic SurveyCambridge UK;</p> <p>Department of EngineeringUniversity of CambridgeCambridge UK;</p> <p>Department of Earth SciencesUniversity of CambridgeCambridge UK;</p> <p>School of Geographical SciencesUniversity of BristolBristol 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=Antarctic&option=203" rel="nofollow">Antarctic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sea ice&option=203" rel="nofollow">sea ice;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=last interglacial&option=203" rel="nofollow">last interglacial;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=128?ka&option=203" rel="nofollow">128?ka;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ice cores&option=203" rel="nofollow">ice cores;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment cores&option=203" rel="nofollow">sediment cores;</a> </p> <div class="translation"> 机译：南极;海冰;最后一个侧面;128？ka;冰核;沉积物核心; 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