The evolution and volcanic forcing of the southern annular mode during the past 300 years

机译：过去300年期间南方环形模式的演变与火山迫使

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ABSTRACT >A positive change in the southern annular mode (SAM), which is the primary pattern of climate variability in the Southern Hemisphere, has been induced predominantly by polar stratospheric ozone depletion. However, the lack of long‐term observational records limits our understanding of the long‐term SAM behaviour. In this study, we found that the geochemical record of the LGB69 ice core from the eastern coast of Antarctica was significantly correlated with the winter SAM index (SAMI). In addition, we developed an annual mean SAMI beginning in 1701 based on 15 annually resolved ice cores and relevant proxy–climate relationships. Our reconstruction accounted for 54.8% of the total variance from 1957 to 2000 (the calibration period). We demonstrate that the recent positive phase shift in the annual mean SAMI since the 1970s is unprecedented, with the estimate for the latest regime in the 1990s reaching values 2.5 times the standard deviation above the baseline (1701–2000). This peak value also coincides with the largest 30‐ and 50‐year trends, which have occurred at the end of the 20th century. From the reconstructed SAMI, we also found that the response to large volcanic events was likely positive in the 3 years after the eruption, but this positive response can be masked by internal climate variability when a strong El Ni?o event occurs in the eruption year. </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”xml：lang =“en”> <title type =“main”>抽象</ title> >一个正面南方环形模式（SAM）的变化，这是南半球气候变异性的主要模式，主要由极地平流层臭氧耗尽主要引起。然而，缺乏长期的观察记录限制了我们对长期斋月行为的理解。在这项研究中，我们发现，来自南极洲东部海岸的LGB69冰芯的地球化学记录与冬季SAM指数（SAMI）显着相关。此外，我们在1701年开始于1701年开发了一年一度的平均萨米，基于每年解决的冰芯和相关的代理气候关系。我们的重建占1957年至2000年总方差的54.8％（校准期）。我们证明，自20世纪70年代以来，最近萨米的阶段阶段阶段偏移是前所未有的，在20世纪90年代的最新制度达到了基线上方标准差值的最新制度估算了2.5倍。这种峰值同样与最大的30至50年趋势一致，在20世纪末发生的最大趋势。从重建的Sami，我们还发现，对大型火山事件的反应可能在爆发后3年内积极，但是当强烈的EL NI突然发生时，这种积极反应可以通过内部气候变化来掩盖。。</ 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-21026/'>《International Journal of Climatology: A Journal of the Royal Meteorological Society》</a> <b style="margin: 0 2px;">|</b><span>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共12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=Yang Jiao&option=202" target="_blank" rel="nofollow">Yang Jiao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xiao Cunde&option=202" target="_blank" rel="nofollow">Xiao Cunde;</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>State Key Laboratory of Cryospheric SciencesNorthwest Institute of Eco‐Environment and Resources Chinese Academy of SciencesLanzhou China;</p> <p>State Key Laboratory of Earth Surface and Source EcologyBeijing Normal UniversityChina;</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/1232.html" title="气候学">气候学;</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=ice core&option=203" rel="nofollow">ice core;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=southern annular mode&option=203" rel="nofollow">southern annular mode;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=reconstruction&option=203" rel="nofollow">reconstruction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcanic forcing&option=203" rel="nofollow">volcanic forcing;</a> </p> <div class="translation"> 机译：南极;冰芯;南方环形模式;重建;火山迫使; </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/0704023002936.html">The evolution and volcanic forcing of the southern annular mode during the past 300 years</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Jiao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yang Jiao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xiao Cunde&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xiao Cunde </a> <a href="/journal-foreign-21026/" target="_blank" rel="nofollow" class="tuijian_authcolor">International Journal of Climatology: A Journal of the Royal Meteorological Society .</a> 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