Temperature extremes in the Argentina central region and their monthly relationship with the mean circulation and <fc xmlns='http://www.wiley.com/namespaces/wiley'>ENSO</fc>ENSO phases

Rusticucci Matilde; Barrucand Mariana; Collazo Soledad

摘要

ABSTRACT xml:id="joc4895-para-0018"> The aim of this study is to analyse the interannual variability of monthly climatic indices of extreme daily temperature in the central‐north region of Argentina throughout a year and its relationship with the atmospheric circulation. The impact of El Ni?o‐Southern Oscillation ( <fc>ENSO</fc> ) over different temperature indices throughout the year is specially analysed. Globally used indices in the 1970–2010 period are utilized for this purpose. The trends of temperature extremes show warming conditions in several months, especially in October and November. In order to find possible forcings of extreme temperature in the region at monthly scale, the co‐variability with other circulation monthly time series such as changes in the intensity of Southern Hemisphere semi‐permanent anticyclones and the intensity of the subtropical jet were studied. The main finding was a systematic shift of the South Atlantic anticyclone towards the west over the decades in June and August, which might hinder the cold advections over the region surveyed. Moreover, the influence of the variation on the intensity of the subtropical jet over extreme events showed significant positive (negative) correlations between the intensity of the jet and the frequency of cold (warm) indices in a great number of months. Finally, the influence of the <fc>ENSO</fc> phases on each of the temperature extremes analysed was studied. It was found that under El Ni?o conditions, minimum temperatures are affected quite evenly throughout the year, fostering the occurrence of warm nights. The impact of the El Ni?o event on the maximum extreme temperatures, however, shows seasonal differences. Between July and September warm days conditions are fostered, while between November and February the </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 =“joc4895-abs-0001”> <标题类型=“main”>抽象</ title> < P XML：ID =“JOC4895-PARA-0018”>本研究的目的是分析一年内阿根廷中北部地区极端日常温度的年度气候索引的年性变化及其与大气流通的关系。 EL NI？O-Southern振荡（<FC> ENSO </ FC>）的影响特别分析了不同的温度指数。 1970 - 2010年期间的全球使用指数用于此目的。极端温度趋势在几个月内显示了温暖的条件，特别是在10月和11月。为了以每月规模找到该地区的极端温度的可能强调，研究了与其他循环月度时间序列的共变性，如南半球半永活链强度的变化和亚热带射流的强度。主要发现是南大西洋反周气通向西部的系统转变，于6月至8月，可能会阻碍对该地区的感冒平流。此外，在极端事件中，亚热带射流强度变化的影响显示了射流强度与大月中的射流强度和冷（温暖）指数之间的显着正（负）相关性。最后，研究了<Fc> Enso </ Fc>相对分析的每个温度极值的相位。结果发现，在EL NI？O条件下，全年的最低温度受到均匀影响，促进了温暖的夜晚的发生。然而，EL NI的影响在最大的极端温度上显示出季节性差异。在7月和9月之间，促进了温暖的日子条件，而11月至2月之间 </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15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=Rusticucci Matilde&option=202" target="_blank" rel="nofollow">Rusticucci Matilde;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barrucand Mariana&option=202" target="_blank" rel="nofollow">Barrucand Mariana;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Collazo Soledad&option=202" target="_blank" rel="nofollow">Collazo Soledad;</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>Departamento de Ciencias de la Atmósfera y los Océanos Facultad de Ciencias Exactas y NaturalesUniversidad de Buenos Aires (DCAO‐FCEN‐UBA)Argentina;</p> <p>Departamento de Ciencias de la Atmósfera y los Océanos Facultad de Ciencias Exactas y NaturalesUniversidad de Buenos Aires (DCAO‐FCEN‐UBA)Argentina;</p> <p>Departamento de Ciencias de la Atmósfera y los Océanos Facultad de Ciencias Exactas y NaturalesUniversidad de Buenos Aires (DCAO‐FCEN‐UBA)Argentina;</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=monthly extreme temperature events&option=203" rel="nofollow">monthly extreme temperature events;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=trends&option=203" rel="nofollow">trends;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=interannual variability ENSO&option=203" rel="nofollow">interannual variability ENSO;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South Atlantic anticyclone&option=203" rel="nofollow">South Atlantic anticyclone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subtropical jet stream&option=203" rel="nofollow">subtropical jet stream;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Argentina&option=203" rel="nofollow">Argentina;</a> </p> <div class="translation"> 机译：每月极端温度事件;趋势;持续的变异enso;南大西洋抗岩;亚热带喷射流;阿根廷; </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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023002893.html">Temperature extremes in the Argentina central region and their monthly relationship with the mean circulation and <fc xmlns="http://www.wiley.com/namespaces/wiley">ENSO</fc>ENSO phases</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rusticucci Matilde&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rusticucci Matilde,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barrucand Mariana&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Barrucand Mariana,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Collazo Soledad&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Collazo Soledad </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> <span>2017</span><span>,第6期</span> </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：在阿根廷中心地区的温度极值及其与平均流通的月度关系和<FC XMLNS =“http://www.wiley.com/namespaces/wiley”> enso </ fc> enso阶段</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023002908.html">Impacts of different <fc xmlns="http://www.wiley.com/namespaces/wiley">ENSO</fc>ENSO flavors and tropical Pacific convection variability ( <fc xmlns="http://www.wiley.com/namespaces/wiley">ITCZ</fc>ITCZ , <fc xmlns="http://www.wiley.com/namespaces/wiley">SPCZ</fc>SPCZ ) on austral summer rainfall in South America, with a focus on Peru</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sulca Juan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sulca Juan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Takahashi Ken&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Takahashi Ken,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Espinoza Jhan‐Carlo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Espinoza Jhan‐Carlo,</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> <span>2018</span><span>,第1期</span> </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：不同<fc xmlns =“http://www.wiley.com/namespaces/wiley”> enso </ fc> enso口味和热带太平洋对流变异性（<fc xmlns =“http://www.wiley.com /命名空间/ wiley“> ITCZ </ FC> ITCZ，<FC XMLNS =”http://www.wiley.com/namespaces/wiley“> spcz </ fc> spcz）在南美洲的澳大利亚夏季降雨上，有一个专注于秘鲁</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025579263.html">How are warm and cool years in the <fc xmlns="http://www.wiley.com/namespaces/wiley">C</fc>C alifornia <fc xmlns="http://www.wiley.com/namespaces/wiley">C</fc>C urrent related to <fc xmlns="http://www.wiley.com/namespaces/wiley">ENSO</fc>ENSO ?</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fiedler Paul C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fiedler Paul C.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mantua Nathan J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mantua Nathan J. </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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Temperature extremes in the Argentina central region and their monthly relationship with the mean circulation and ENSOENSO phases

摘要