Analysis of the airflow at the centre of the upper plateau on the Iberian Peninsula and its link to CO <sub xmlns='http://www.wiley.com/namespaces/wiley'>2</sub>2 and CH <sub xmlns='http://www.wiley.com/namespaces/wiley'>4</sub>4 concentrations

Pérez Isidro A.; Sánchez M. Luisa; García M. ángeles; Pardo Nuria; Fernández‐Duque Beatriz

摘要

ABSTRACT > Air trajectories are useful tools to investigate the airflow and transport of substances released into the atmosphere. Web‐based models are widely used to calculate trajectories reaching places that are being studied. This article considers 6 years of air trajectories as of October 2010 together with CO <sub>2</sub> and CH <sub>4</sub> concentrations. A bivariate smoothing function that employs the radial distance and direction of the trajectory to the measuring site was used to form trajectory groups from the minima of this function. Varied radial and angular windows were assayed to investigate the behaviour of the smoothing function. Curves associated with the number of minima were L‐shaped and the windows selected corresponded to the ‘knee’ of the curves. Seven trajectory groups were considered to observe the response of the procedure against the radial distance and the direction. Seasonal evolution revealed the greatest radial extent for winter and the lowest for summer. Moreover, trajectories from the Atlantic Ocean were the most frequent. CO <sub>2</sub> and CH <sub>4</sub> concentrations were detrended using a linear function, and average trends were 2.34 and 0.0085 ppm year ?1 , respectively. Annual cycles of detrended concentrations were very soft and were linked to the site's ecosystem. CO <sub>2</sub> presented one maximum in spring linked to substantial vegetation growth, and one minimum in summer, when vegetation dies and dispersion is maximum. CH <sub>4</sub> maximum was observed in winter although the minimum was found in summer and attributed to oxidation with the hydroxyl radical in the troposphere and to dispersion in this season. Analysis of concentration trends for </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> >空气轨迹是调查气流和释放到大气中的物质的运输的有用工具。基于Web的模型被广泛用于计算到达正在研究的地方的轨迹。本文认为，2010年10月与CO <Sub> 2 </ sub>和CH <sub> 4 </ sub>浓度一起考虑6年的空气轨迹。使用与测量部位的轨迹的径向距离和方向采用径向距离和方向的双变化的平滑功能用于从该功能的最小值形成轨迹组。测定各种径向和角度窗口以研究平滑功能的行为。与最小值的数量相关的曲线是L形，并且选择的窗口与曲线的“膝盖”相对应。被认为七个轨迹组观察程序对径向距离和方向的响应。季节性进化显示冬季最大的径向范围，夏季最低。此外，大西洋的轨迹是最常见的。使用线性函数对CO <sub> 2 </ sub>和CH <sub> 4 </ sub>浓度进行了缩小，并且平均趋势分别为2.34和0.0085ppm 1 </ sup>。减去浓度的年度循环非常柔软，与该网站的生态系统相关联。 CO <sub> 2 </ sub>在弹簧中呈现一个最大的植被生长，夏季最少，当植被死亡和分散最大时。在冬季观察到CH <sub> 4 </ sub>最大值，尽管在夏季发现最低并归因于对流层中的羟基氧化并在本赛季分散。集中趋势分析 </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=Pérez Isidro A.&option=202" target="_blank" rel="nofollow">Pérez Isidro A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sánchez M. Luisa&option=202" target="_blank" rel="nofollow">Sánchez M. Luisa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=García M. ángeles&option=202" target="_blank" rel="nofollow">García M. ángeles;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pardo Nuria&option=202" target="_blank" rel="nofollow">Pardo Nuria;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fernández‐Duque Beatriz&option=202" target="_blank" rel="nofollow">Fernández‐Duque Beatriz;</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>Department of Applied Physics Faculty of SciencesUniversity of ValladolidSpain;</p> <p>Department of Applied Physics Faculty of SciencesUniversity of ValladolidSpain;</p> <p>Department of Applied Physics Faculty of SciencesUniversity of ValladolidSpain;</p> <p>Department of Applied Physics Faculty of SciencesUniversity of ValladolidSpain;</p> <p>Department of Applied Physics Faculty of SciencesUniversity of ValladolidSpain;</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=METEX&option=203" rel="nofollow">METEX;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=air trajectory&option=203" rel="nofollow">air trajectory;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbon dioxide&option=203" rel="nofollow">carbon dioxide;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=methane&option=203" rel="nofollow">methane;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=kernel density&option=203" rel="nofollow">kernel density;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=GHG trend&option=203" rel="nofollow">GHG trend;</a> </p> <div class="translation"> 机译：Metex;空气轨迹;二氧化碳;甲烷;核密度;温室气体趋势; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023002961.html">Analysis of the airflow at the centre of the upper plateau on the Iberian Peninsula and its link to CO <sub xmlns="http://www.wiley.com/namespaces/wiley">2</sub>2 and CH <sub xmlns="http://www.wiley.com/namespaces/wiley">4</sub>4 concentrations</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pérez Isidro A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pérez Isidro A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sánchez M. 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Analysis of the airflow at the centre of the upper plateau on the Iberian Peninsula and its link to CO 22 and CH 44 concentrations

摘要

Analysis of the airflow at the centre of the upper plateau on the Iberian Peninsula and its link to CO ₂2 and CH ₄4 concentrations