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Antarctic temperature variability and change from station data

机译:南极温度可变性和站数据的变化

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摘要

Abstract > Variability and change in near‐surface air temperature at 17 Antarctic stations is examined using data from the SCAR READER database. We consider the relationships between temperature, and atmospheric circulation, sea ice concentration and forcing by the tropical oceans. All 17 stations have their largest inter‐annual temperature variability during the winter and the annual mean temperature anomalies are dominated by winter temperatures. The large inter‐annual temperature variability on the western Antarctic Peninsula has decreased over the instrumental period as sea ice has declined. Variability in the phase of the SAM exerts the greatest control of temperatures, although tropical Pacific forcing has also played a large part, along with local atmospheric circulation variability at some locations. The relationship of positive (negative) SAM and high (low) Peninsula and low (high) East Antarctic temperatures was not present before the mid‐1970s. Thirteen of the 17 stations have experienced a positive trend in their annual mean temperature over the full length of their record, with the largest being at Vernadsky (formerly Faraday) (0.46°?±?0.15°C·dec ?1 ) on the western side of the Antarctic Peninsula. The deepening of the Amundsen Sea low as a result of the more positive SAM and changes in the IPO and PDO have contributed to the warming of the Peninsula. Beyond the Antarctic Peninsula there has been little significant change in temperature. The two plateau stations had a small cooling from the late 1970s to the late 1990s consistent with the SAM becoming positive, but have subsequently warmed. During spring there has been an Antarctic‐wide warming, with all but one station having experienced an increase in temperature, although the only trends that were significant were at Vostok, Scott base, Vernadsky and Amundsen‐Scott. In this season, much of the Peninsula/West Antarctic warming can be attributed to tropical Pacific forcing through the IPO/PDO. </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:Lang =“en”> <标题类型=“main”>抽象</ title> > 使用来自瘢痕读卡器数据库的数据检查17个南极站的近表面空气温度的变异性和变化。我们考虑温度与大气循环之间的关系,海冰浓度和热带海洋强迫。所有17个站都在冬季的年度最大的年度温度变异性,年均平均温度异常是由冬季温度的主导。随着海冰率下降,西南极半岛的大型年度温度变异性在乐器时期下降。虽然热带太平洋强迫也在一些地点,但是,山姆阶段的变化施加了最大的温度控制,尽管热带太平洋强迫也发挥了很大的作用,以及某些地方的局部大气循环变异。在20世纪70年代中期之前,阳性(负)山姆和高(低)半岛和低(高)东南南极温度的关系。 17个站的十三个站在他们的年度平均温度上遇到了积极趋势,在全长的记录中,最大的是Vernadsky(前者前)(0.46°?±0.15°C·DEC ?1 </ sup> )在南极半岛的西侧。由于山姆更积极的山姆和IPO和PDO的变化,大蒙森鲈的深化导致半岛的变暖。除了南极半岛之外,温度几乎没有显着变化。这两个高原站从20世纪70年代后期到20世纪90年代后期的高原冷却符合山姆的积极态度,但随后被温暖了。春季期间,一直是南极宽的变暖,除了一个驻地的温度增加,尽管唯一的趋势是Vostok,Scott Base,Vernadsky和Amundsen-Scott。在本赛季,大部分半岛/西南极变暖都可以归因于热带太平洋,通过IPO / PDO强制强迫。 </ p> </摘要> </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>2020年第6期</span><b style="margin: 0 2px;">|</b><span>共22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=Turner John&option=202" target="_blank" rel="nofollow">Turner John;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marshall Gareth J.&option=202" target="_blank" rel="nofollow">Marshall Gareth J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Clem Kyle&option=202" target="_blank" rel="nofollow">Clem Kyle;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Colwell Steve&option=202" target="_blank" rel="nofollow">Colwell Steve;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Phillips Tony&option=202" target="_blank" rel="nofollow">Phillips Tony;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lu Hua&option=202" target="_blank" rel="nofollow">Lu Hua;</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 SurveyNatural Environment Research CouncilCambridge UK;</p> <p>British Antarctic SurveyNatural Environment Research CouncilCambridge UK;</p> <p>Institute of Earth Ocean and Atmospheric Sciences Rutgers UniversityNew Brunswick New Jersey;</p> <p>British Antarctic SurveyNatural Environment Research CouncilCambridge UK;</p> <p>British Antarctic SurveyNatural Environment Research CouncilCambridge UK;</p> <p>British Antarctic SurveyNatural Environment Research CouncilCambridge 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/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=Antarctica&option=203" rel="nofollow">Antarctica;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=climate change&option=203" rel="nofollow">climate change;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=climate variability&option=203" rel="nofollow">climate variability;</a> <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> </p> <div class="translation"> 机译:南极洲;气候变化;气候变异性;温度; 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LiYan</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李燕&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李燕</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Bowen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Liu Bowen</a> <span> <a href="/conference-cn-2200/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2014年全国气象观测技术交流会 </a> <span> <span> . 2014</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020315753167.html">基于热红外和被动微波数据的南极冰盖冰雪表面温度反演和变化研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李亚超&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李亚超</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120112023149.html">基于多地面站数据的GNSS功率变化时刻自动分析方法</a> <b>[P]</b> . <span> 中国专利: CN112014863A </span> <span> . 2020-12-01</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120595307.html">根据导频信号的时间变化过程向接收站传输数据的方法</a> <b>[P]</b> . <span> 中国专利: CN100592658C </span> <span> . 2010.02.24</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130426862062.html">DATA EXCHANGE METHOD, DATA EXCHANGE SYSTEM AND DATA EXCHANGE STATION</a> <b>[P]</b> . <span> 外国专利: <!-- 俄罗斯专利: --> RU2387087C2 </span> <span> . 2010-04-20</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译:数据交换方法,数据交换系统和数据交换站 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130439055457.html">Method for channel configuration at transmission of data over broadcast networks, 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initial;text-overflow: initial;overflow: initial;"> <span>机译:电子控制主站的分支交换-冗余数据通道连接到备用控制站,以覆盖主交换故障的可能性 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023003293','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉,该期刊暂不可订阅,敬请期待!</p> <p class="current">目前支持订阅全部北京大学中文核心(2020)期刊目录。</p> <div style="display: flex;margin-top: 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