Reconstructed annual mean temperatures for the northeastern margin of the Tibetan Plateau: associations with the East Asian monsoons and volcanic events

Wang Bo; Chen Tuo; Xu Guobao; Wu Guoju; Li Caijuan

摘要

ABSTRACT xml:id="joc4900-para-0008"> Owing to a lack of available long‐term climatic records, data related to past climatic variability throughout the Tibetan Plateau remains limited. In this study, we found that Qilian juniper tree growth was significantly and positively correlated ( <fi>p</fi> ??0.001) to yearly mean temperatures in the northeastern margin of the Tibetan Plateau. We developed an annual mean temperature reconstruction from year 1740? <fc>CE</fc> based on growth‐climate relationships in the study area. Our reconstruction accounted for 53.9% of total variance from 1956 to 2012 (the calibration period). Through this reconstruction, we were successfully able to capture recent abrupt climate change events that generally agreed with other temperature‐sensitive tree‐ring reconstructions on both regional and hemisphere scales under a decadal timescale. Periods from 1820 to 1830, 1855 to 1890, and 1960 to 1985? <fc>CE</fc> corresponded to cold periods in the reconstruction, while the 1740s and periods from 1795 to 1815 and from 1990 to 2012? <fc>CE</fc> corresponded to relatively warm periods. We also detected increased interannual change variability in annual mean temperatures since the 1980s, which could be related to increasing variability in the East Asian winter monsoon as well as the rapid climate warming that has occurred since this time. From these reconstructed temperatures, we were successfully able to capture the occurrences of large volcanic events in China as well as five historic volcanic events outside China that had global implications on climate variability and that resulted in planetary cooling during the period from 1740 to 2012? <fc>CE</fc> . This in turn suggested that these volcanic events woul </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：id =“joc4900-abs-0001”> <标题类型=“main”>抽象</ title> < P XML：ID =“Joc4900-Para-0008”>由于缺乏可用的长期气候记录，与过去的藏高高原过去的气候变异有关的数据仍然有限。在这项研究中，我们发现祁连杜松树的生长显着且呈正相关（<fi> p </ fi>＆ 0.001）到藏高原东北边缘的年平均温度。我们从1740年开发了年度平均温度重建？ <FC> CE </ FC>基于研究区域的生长气候关系。我们的重建占1956年至2012年总方差的53.9％（校准期）。通过这种重建，我们成功地捕获了近期突然的气候变化事件，这些事件通常同意在划分的时间尺度下区域和半球鳞片上的其他温度敏感的树木重建。 1820年至1830年，1855年至1890年，1960年至1985年的时期？ <FC> CE </ FC>对应于重建中的寒流，而1790年至1815年和1990年至2012年的1740年代和期间？ <FC> CE </ FC>对应于相对温暖的时期。我们还检测到自20世纪80年代以来年平均温度的持续变化变化增加，这可能与东亚冬季季风的越来越多的变异有关，以及自此次时间以来发生的快速气候变暖。从这些重建的温度来看，我们成功地捕获了中国大型火山场事件的发生，以及中国以外的五个历史火山活动，对气候变异性具有全球影响，并导致行星冷却在1740年至2012年期间？ <FC> CE </ FC>。这反过来建议这些火山事件乏味 </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>2017年第6期</span><b style="margin: 0 2px;">|</b><span>共13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=Wang Bo&option=202" target="_blank" rel="nofollow">Wang Bo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Tuo&option=202" target="_blank" rel="nofollow">Chen Tuo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Guobao&option=202" target="_blank" rel="nofollow">Xu Guobao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu Guoju&option=202" target="_blank" rel="nofollow">Wu Guoju;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Caijuan&option=202" target="_blank" rel="nofollow">Li Caijuan;</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 Science Northwest Institute of Eco‐Environment and ResourcesChinese Academy of SciencesLanzhou China;</p> <p>State Key Laboratory of Cryospheric Science Northwest Institute of Eco‐Environment and ResourcesChinese Academy of SciencesLanzhou China;</p> <p>State Key Laboratory of Cryospheric Science Northwest Institute of Eco‐Environment and ResourcesChinese Academy of SciencesLanzhou China;</p> <p>State Key Laboratory of Cryospheric Science Northwest Institute of Eco‐Environment and ResourcesChinese Academy of SciencesLanzhou China;</p> <p>State Key Laboratory of Cryospheric Science Northwest Institute of Eco‐Environment and ResourcesChinese Academy of SciencesLanzhou China;</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=temperature&option=203" rel="nofollow">temperature;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=variability&option=203" rel="nofollow">variability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tree ring&option=203" rel="nofollow">tree ring;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=dendroclimatology&option=203" rel="nofollow">dendroclimatology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=potential driver&option=203" rel="nofollow">potential driver;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tibetan Plateau&option=203" rel="nofollow">Tibetan Plateau;</a> </p> <div class="translation"> 机译：温度;变异性;树圈;树突状况;潜在的司机;藏高原; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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" 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