首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Cloud transitions: comparison of temporal variation in the southeastern Pacific with the spatial variation in the northeastern Pacific at low latitudes
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Cloud transitions: comparison of temporal variation in the southeastern Pacific with the spatial variation in the northeastern Pacific at low latitudes

机译:云转换:东南太平洋地区季节变异与东北太平洋低纬度的空间变化比较

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ABSTRACT xml:id="joc4889-para-0001"> The seasonal variation of clouds in the southeastern equatorial Pacific ( <fc>SEP</fc> ) is analysed and compared with the spatial variation of clouds in the northeastern Pacific along the Global Energy and Water Cycle Experiment Cloud System Study/Working Group on Numerical Experimentation ( <fc>GCSS</fc> / <fc>WGNE</fc> ) Pacific Cross‐Section Intercomparison ( <fc>GPCI</fc> ) transect. A ‘seasonal cloud transition’?–?from stratocumulus to shallow cumulus and eventually to deep convection?–?is found in the <fc>SEP</fc> from September to April, which is similar to the spatial cloud transition along the <fc>GPCI</fc> transect from the California coast to the equator. It is shown that this seasonal cloud transition in the <fc>SEP</fc> is associated with increasing sea surface temperature ( <fc>SST</fc> ), decreasing lower tropospheric stability and large‐scale subsidence, which are all similar to the spatial variation of these fields along the <fc>GPCI</fc> transect. Difference is found that the <fc>SEP</fc> cloud transition is associated with decreasing surface wind speed and surface latent heat flux, weaker larger‐scale upward motion and convective instability, which lead to less deepening of the low clouds and less frequent deep convection than those in the <fc>GPCI</fc> transect. The seasonal cloud transition in the <fc>SEP</fc> provides a test for climate models to simulate the relationships between clouds and large‐scale atmospheric fields in a region that features a spurious double inter‐tropical convergence zone ( <fc>ITCZ</fc> ) in most m </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 =“joc4889-abs-0001”> <标题类型=“main”>抽象</ title> < P XML:ID =“JOC4889-PARA-0001”>分析了东南赤道太平洋(<FC> SEP </ FC>)的季节变化,并与全球东北太平洋云的空间变化相比能源和水循环实验云系统研究/工作组关于数值实验(<FC> GCSS </ FC> / <FC> WGNE </ FC>)太平洋横截面相应(<FC> GPCI </ FC>)横断。 '季节性云转换' - ?从划分为浅层,最终到深入对流? - ?是在9月到4月的<fc> sep </ fc>中发现,它类似于沿着空间云转换FC> GPCI </ FC>从加利福尼亚州海岸横断到赤道。结果表明,这种季节性云转换在<FC> SEP </ FC>中与海面温度(<FC> SST </ FC>)增加,降低了对流层稳定性和大规模沉降,这都是相似的沿<FC> GPCI </ FC>横断之间这些字段的空间变化。差异发现,<FC> SEP </ FC>云转变与表面风速和表面潜热通量的降低相关,较大尺度向上运动和对流不稳定性,这导致低云层的加深且较少的频繁深度对流比<FC> GPCI </ FC>横断面的对流。 <FC> SEP </ FC>中的季节性云转换为气候模型提供了一种测试,以模拟具有伪装双层热带收敛区(<FC> ITCZ的区域中的云和大型大气领域之间的关系(<FC> ITCZ) </ fc>)在大多数m </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11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=Yu Haiyang&option=202" target="_blank" rel="nofollow">Yu Haiyang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Minghua&option=202" target="_blank" rel="nofollow">Zhang Minghua;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lin Wuyin&option=202" target="_blank" rel="nofollow">Lin Wuyin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Xiaoxiao&option=202" target="_blank" rel="nofollow">Zhang Xiaoxiao;</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>School of Marine and Atmospheric SciencesStony Brook UniversityNY USA;</p> <p>School of Marine and Atmospheric SciencesStony Brook UniversityNY USA;</p> <p>Brookhaven National LaboratoryUpton NY USA;</p> <p>ICCESInstitute of Atmospheric Physics (IAP) Chinese Academy of SciencesBeijing 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=cloud transition&option=203" rel="nofollow">cloud transition;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=GPCI&option=203" rel="nofollow">GPCI;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=southeastern equatorial Pacific&option=203" rel="nofollow">southeastern equatorial Pacific;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=marine boundary layer&option=203" rel="nofollow">marine boundary layer;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=deep convection&option=203" rel="nofollow">deep convection;</a> </p> <div class="translation"> 机译:云转换;GPCI;东南赤道太平洋;海洋边界层;深入对流; </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" href="/journal-foreign-detail/0704023002891.html">Cloud transitions: comparison of temporal variation in the southeastern Pacific with the spatial variation in the northeastern Pacific at low latitudes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Haiyang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yu Haiyang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Minghua&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Minghua,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lin Wuyin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lin Wuyin,</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:云转换:东南太平洋地区季节变异与东北太平洋低纬度的空间变化比较</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_estuarine-coastal-and-shelf-science_thesis/0204113432657.html">Spatial-temporal variations in echinoderm diversity within coral communities in a transitional region of the northeast of the eastern pacific</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sotelo-Casas R. 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<span> 外国专利: <!-- --> CA2842594A1 </span> <span> . 2013-01-31</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:确定非均相系统中蛋白水解酶活性的时空分布的方法(变体),实现该装置的方法和基于空间和温度变化的诊断系统中的缺陷的方法非均相系统中蛋白水解酶的活性 </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('0704023002891','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 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