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The Role of Oceanic Processes in the Initiation of Indian Summer Monsoon Intraseasonal Oscillations Over the Indian Ocean

机译：海洋过程在印度夏季季风在印度洋初始振荡中的作用

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Abstract >Observational analyses and a hierarchy of ocean general circulation model (OGCM) experiments were performed to understand the influence of oceanic processes on the warm sea surface temperature anomalies (SSTAs) prior to the convection initiation of Indian summer monsoon intraseasonal oscillations (MISOs) in the equatorial Indian Ocean. Satellite observations revealed 41 strong MISO events that initiated over the central equatorial Indian Ocean and propagated northward to the Indian subcontinent and/or eastward to the Maritime Continent during the May–October season of the 2001–2012 period. Eight of those events were preceded by SSTAs that were strongly influenced by wind stress‐driven oceanic processes. Composite analyses for the eight events showed that more than one‐third of the preconvection warming in the initiation region resulted from oceanic processes, including advection and entrainment. Case studies of two strong MISO events associated with ocean‐dynamically induced SSTAs showed unmistakable evidence for the preconvection SSTAs and sea surface height anomalies (SSHAs) associated with eastern boundary‐reflected (in June/July 2004) and directly forced (in June 2006) intraseasonal oceanic Rossby waves. In those two case studies, a mixed‐layer heat budget analysis of the OGCM results showed that advection played a much larger role than entrainment in elevating SSTAs. Further analysis showed that intraseasonal currents associated with the Rossby waves advected high seasonal mean SSTs into the initiation region. As current forecasting skills for the onset of the MISO are low, these results underscore the importance of thoroughly understanding the ocean's role in affecting SSTAs, which contribute to MISO initiation. </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”> <标题类型=“main”>抽象</ title> >观察分析和海洋一般循环模型（OGCM）实验的层次结构，以了解海洋过程对温暖的影响海面温度异常（SSTA）在赤道印度洋中印度夏季季风的对流发起之前的对流发起震荡（Misos）。卫星观察显示，在中央赤道印度洋中发起的41个强烈的味噌事件，并在2001 - 2012年5月期间，在2001 - 2012年5月期间向印度次大陆和/或向东传播到海洋大陆。这些事件中的八个事件是由风力应激驱动的海洋过程强烈影响的SSTA。八个事件的复合分析表明，从海洋过程中导致了起始区域中的超过三分之一的预升温，包括平流和夹带。对与海洋动态诱导的SSTA相关的两个强味噌事件的案例研究表明，与东部边界反映的前视SSTA和海面高度异常（SSHA）显示了明确证据（2004年6月/ 7月）并直接强迫（2006年6月）陷入困境的海洋rossby波。在这两个案例研究中，OGCM结果的混合层热预算分析表明，平流在提升SSTA中的夹带中发挥了更大的作用。进一步的分析表明，与Rossby波相关的季节性电流对起始区域的高季节性平均值进行了建立。由于目前的味噌发作的预测技能是低的，这些结果强调了彻底了解海洋在影响SSTA方面的作用的重要性，这有助于味噌启动。</ 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-34643/'>《Journal of Geophysical Research, C. Oceans: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第5期</span><b style="margin: 0 2px;">|</b><span>共20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=West B. Jason&option=202" target="_blank" rel="nofollow">West B. Jason;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Han Weiqing&option=202" target="_blank" rel="nofollow">Han Weiqing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Yuanlong&option=202" target="_blank" rel="nofollow">Li Yuanlong;</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 Atmospheric and Oceanic SciencesUniversity of ColoradoBoulder Colorado USA;</p> <p>Department of Atmospheric and Oceanic SciencesUniversity of ColoradoBoulder Colorado USA;</p> <p>Department of Atmospheric and Oceanic SciencesUniversity of ColoradoBoulder Colorado USA;</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=oceanic processes&option=203" rel="nofollow">oceanic processes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rossby waves&option=203" rel="nofollow">Rossby waves;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Indian summer monsoon&option=203" rel="nofollow">Indian summer monsoon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=intraseasonal oscillations&option=203" rel="nofollow">intraseasonal oscillations;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=air‐sea interaction&option=203" rel="nofollow">air‐sea interaction;</a> </p> <div class="translation"> 机译：海洋过程;Rossby波;印度夏季季风;陷入困境的振荡;海运互动; </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> <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/0704025579252.html">The Role of Oceanic Processes in the Initiation of Indian Summer Monsoon Intraseasonal Oscillations Over the Indian Ocean</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=West B. 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