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首页> 外文期刊>Geophysical Research Letters >Mechanisms of Northward Propagation of Boreal Summer Intraseasonal Oscillation Revealed by Climate Model Experiments
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Mechanisms of Northward Propagation of Boreal Summer Intraseasonal Oscillation Revealed by Climate Model Experiments

机译:气候模型实验展示北方夏季北欧震荡的北方传播机制

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Abstract >Northward propagation of the boreal summer intraseasonal oscillation (ISO) has profound impacts on Northern Hemisphere extreme weather events. This study aims to test the hypotheses proposed in the previous studies to explain northward propagation of the ISO by drastically changing the climatological mean states through lowering the Tibetan Plateau (TP) with a fully coupled Earth system model, Nanjing University of Information Science and Technology Earth System Model version 3.0. The model reproduces realistic ISO over South Asia and the northern Indian Ocean. The results show that ISO northward propagations significantly weaken with decreased elevation of the TP. Lowering the TP reduces the vertical shear of the mean monsoon circulation over the northern Indian Ocean. The reduced vertical shear deteriorates the generation of positive vorticity anomalies and boundary layer moisture convergence to the north of ISO precipitation center, thereby weakening northward propagation of the ISO. On the other hand, the boundary layer moisture advection and air‐sea interaction do not change appreciably when the TP elevation is reduced. These results suggest that the mean state vertical shear is most critical for the ISO northward propagation. </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><抽象类型=“主要”的xml:郎=“EN”> <标题类型=“主”>抽象</ TITLE> <P>寒带夏季季节内振荡(ISO)的向北传播对北半球极端天气产生深远的影响事件。这项研究旨在测试在以前的研究中提出的假设,通过与完全耦合地球系统模型,信息科学与技术地球南京大学降低青藏高原(TP)急剧变化的气候平均状态来解释ISO的北传系统模型3.0版。该模型再现了南亚和印度洋北部现实ISO。结果表明,ISO向北的传播显著与TP的海拔下降削弱。降低TP降低了平均季风环流在印度洋北部的垂直切变。减小的垂直切变恶化正涡异常和边界层湿气收敛的生成以ISO沉淀中心的北,从而削弱了ISO向北传播。在另一方面,边界层水汽平流和海气相互作用不会明显改变时,TP高程降低。这些结果表明,平均状态垂直切变是为ISO向北传播最关键的。</ p> </抽象> </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2019年第6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=Yang Young‐Min&option=202" target="_blank" rel="nofollow">Yang Young‐Min;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Bin&option=202" target="_blank" rel="nofollow">Wang Bin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lee June‐Yi&option=202" target="_blank" rel="nofollow">Lee June‐Yi;</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>Key Laboratory of Meteorological Disaster of Ministry of Education and Earth System Modeling CenterNanjing University of Information Science and TechnologyNanjing China;</p> <p>Key Laboratory of Meteorological Disaster of Ministry of Education and Earth System Modeling CenterNanjing University of Information Science and TechnologyNanjing China;</p> <p>Research Center for Climate Sciences and Department of Climate SystemPusan National UniversityBusan South Korea;</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/163.html" title="地球物理学">地球物理学;</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=ISO&option=203" rel="nofollow">ISO;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ISO northward propagation&option=203" rel="nofollow">ISO northward propagation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=boreal summer ISO (BSISO)&option=203" rel="nofollow">boreal summer ISO (BSISO);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ISO simulation&option=203" rel="nofollow">ISO simulation;</a> </p> <div class="translation"> 机译:ISO;ISO向北传播;Boreal Summer ISO(BSISO);ISO仿真; 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