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首页> 外文期刊>Journal of quaternary science: JQS >Moisture variations in arid central Asia and its out‐of‐phase relationship with the Asian Monsoon during MIS 5: evidence from loess records
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Moisture variations in arid central Asia and its out‐of‐phase relationship with the Asian Monsoon during MIS 5: evidence from loess records

机译：干旱中亚的水分变化及其与亚洲季风在MIS 5期间与亚洲季风的关系变化：来自黄土记录的证据

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ABSTRACT <section xml:id="jqs3024-sec-0001"> >An out‐of‐phase relationship between moisture variations in arid central Asia (ACA) and Monsoon Asia is revealed in various Holocene sedimentary records. To determine whether this relationship also occurred during previous warm intervals, we reconstructed the history of moisture variations during Marine Isotope Stage 5 (MIS 5) recorded in a loess profile from the Yili valley in the Tienshan Mountains, in ACA, and compared it with the record from the Chinese Loess Plateau (CLP). Three humid episodes in the Yili valley are recorded, at 72–79.5, 93.5–101 and 113.5–125.5 ka; in addition, intervals of fine grain size, indicating a low incidence of dust storms, and thus low ice volume in the Northern Hemisphere, occurred during 76–83.5, 97–106 and 117.5–130 ka. Our findings indicate that during MIS 5, variations in humidity in ACA lagged (by ～3–5 ka) variations in the Asian Monsoon recorded by magnetic and grain‐size proxies from the CLP. Furthermore, we propose that precipitation variations in ACA were negatively correlated with the intensity of the Asian Monsoon because of corresponding movements in pressure and rain belts, and were positively correlated with sea surface temperature variations in the North Atlantic. </section> </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> <section XML：ID =“JQS3024-SEC-0001”> >在各种全新世沉积记录中揭示了干旱中亚（ACA）和季风亚洲的水分变化之间的相位关系。为了确定此关系是否也发生在以前的热间隔期间，我们在海洋同位素第5阶段5（MIS 5）期间重建了水分变化的历史，从蒂伊山山脉的黄土山脉，在ACA中，并与之比较了从中国黄土高原（CLP）记录。 yili山谷中的三张潮湿的剧集被记录在72-79.5,93.5-101和113.5-125.5 Ka;此外，细粒尺寸的间隔，表明北半球的尘埃风暴的低发生率，以及北半球的低冰量，发生在76-83.5,97-106和117.5-130 ka期间。我们的研究结果表明，在MIS 5期间，ACA湿度的变化滞后（通过磁性和晶粒尺寸代理从CLP记录的亚洲季风的变化。此外，由于压力和雨风带的相应运动，我们提出了ACA的降水变化与亚洲季风的强度负相关，并且与北大西洋的海面温度变化正相关。</ p> </截面呈正相关。</ p> </ section > </ 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-35770/'>《Journal of quaternary science: JQS》</a> <b style="margin: 0 2px;">|</b><span>2018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=Jia Jia&option=202" target="_blank" rel="nofollow">Jia Jia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fuyuan Gao&option=202" target="_blank" rel="nofollow">Fuyuan Gao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dunsheng Xia&option=202" target="_blank" rel="nofollow">Dunsheng Xia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei Huang&option=202" target="_blank" rel="nofollow">Wei Huang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fahu Chen&option=202" target="_blank" rel="nofollow">Fahu Chen;</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>MOE Key Laboratory of West China's Environmental System College of Earth and Environmental SciencesLanzhou UniversityLanzhou China;</p> <p>MOE Key Laboratory of West China's Environmental System College of Earth and Environmental SciencesLanzhou UniversityLanzhou China;</p> <p>MOE Key Laboratory of West China's Environmental System College of Earth and Environmental SciencesLanzhou UniversityLanzhou China;</p> <p>MOE Key Laboratory of West China's Environmental System College of Earth and Environmental SciencesLanzhou UniversityLanzhou China;</p> <p>MOE Key Laboratory of West China's Environmental System College of Earth and Environmental SciencesLanzhou UniversityLanzhou 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/27341.html" title="第四纪（系）">第四纪（系）;</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=arid central Asia&option=203" rel="nofollow">arid central Asia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=loess–paleosol sequence&option=203" rel="nofollow">loess–paleosol sequence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=MIS 5&option=203" rel="nofollow">MIS 5;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=out‐of‐phase moisture variations&option=203" rel="nofollow">out‐of‐phase moisture variations;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Westerlies&option=203" rel="nofollow">Westerlies;</a> </p> <div class="translation"> 机译：中亚干旱;黄土 - 古溶解序列;MIS 5;超阶段的水分变化;韦斯特利; 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