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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Assessment of western II ndian OO cean SSTSST bias of CMIP5CMIP5 models
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Assessment of western II ndian OO cean SSTSST bias of CMIP5CMIP5 models

机译：西方的评估 i i NDian. O o 芯片 sst sst 偏见 cmip5 cmip5 楷模

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Abstract >The western Indian Ocean sea surface temperature (SST) is among the key factors that affect precipitation over India and East Africa. This study examined the western Indian Ocean SST biases among the Coupled Model Intercomparison Project phase 5 (CMIP5) models. It was found that the multimodel ensemble‐mean SST biases over the western equatorial Indian Ocean are warmer than the observations during the summer monsoon season. However, about half the models show positive SST biases, whereas negative ones in the other half. The models with warmer SST biases exhibit a pattern similar to the Indian Ocean Dipole, with stronger equatorial easterly wind biases during fall and a deeper thermocline in the western equatorial Indian Ocean. In the models with cooler SST biases, negative SST biases are observed over the entire tropical Indian Ocean throughout the year and the wind biases over the equatorial Indian Ocean are southeasterly during summer and fall. Heat budget analysis revealed the importance of ocean currents in forming the early summer development of SST biases over the western equatorial Indian Ocean. The formation of SST biases is related to surface current biases induced by the weaker biases of southwesterly monsoon winds and SST biases over the southwestern equatorial Indian Ocean, which are advected by the East African Coastal Currents. On the other hand, almost of all the CMIP5 models show prominent cold SST biases over the northern Arabian Sea during the premonsoon season. The SST biases are induced by excess surface cooling during the winter monsoon season. </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 xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”> <标题类型=“main”>抽象</ title> <P>西印度洋海洋海景（SST）是影响印度和东非降水的关键因素。本研究检测了耦合型号相互熟悉项目阶段5（CMIP5）模型中的西部印度洋SST偏见。结果发现，西赤道印度洋的Multimodel合奏 - 意思是SST偏见比夏季季风季节的观察更温暖。然而，大约一半的模型显示出积极的SST偏见，而另一半的负面情况。具有较高的SST偏见的型号表现出类似于印度洋偶极子的模式，在秋季期间具有更强的赤道东风偏见，在西部赤道印度洋中的更深层次的热量下划线。在具有较冷的SST偏差的模型中，整个热带印度洋观察到阴性SST偏差，在夏季和秋季赤道印度洋的风偏差是东南。热预算分析揭示了海洋电流在西部赤道印度洋中SST偏见的初夏发展的重要性。 SST偏差的形成与由东南赤道印度海洋的西南季风风和SST偏差的偏弱引起的表面电流偏差有关。另一方面，几乎所有的CMIP5模型都在预先发生的季节显示了北阿拉伯海洋上的显着冷酷的SST偏见。 SST偏置在冬季季风季节过多的表面冷却诱导。</ 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>2017年第4期</span><b style="margin: 0 2px;">|</b><span>共18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=Fathrio Ibnu&option=202" target="_blank" rel="nofollow">Fathrio Ibnu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iizuka Satoshi&option=202" target="_blank" rel="nofollow">Iizuka Satoshi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Manda Atsuyoshi&option=202" target="_blank" rel="nofollow">Manda Atsuyoshi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kodama Yasu‐Masa&option=202" target="_blank" rel="nofollow">Kodama Yasu‐Masa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ishida Sachinobu&option=202" target="_blank" rel="nofollow">Ishida Sachinobu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moteki Qoosaku&option=202" target="_blank" rel="nofollow">Moteki Qoosaku;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamada Hiroyuki&option=202" target="_blank" rel="nofollow">Yamada Hiroyuki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tachibana Yoshihiro&option=202" target="_blank" rel="nofollow">Tachibana Yoshihiro;</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>Meteorological Laboratory Graduate School of Science and TechnologyHirosaki UniversityHirosaki Aomori Japan;</p> <p>Storm Flood and Landslide DivisionNational Research Institute for Earth Science and Disaster ResilienceTsukuba Ibaraki Japan;</p> <p>Climate and Ecosystems Dynamics Division Graduate School of BioresourcesMie UniversityTsu Mie Japan;</p> <p>Meteorological Laboratory Graduate School of Science and TechnologyHirosaki UniversityHirosaki Aomori Japan;</p> <p>Meteorological Laboratory Graduate School of Science and TechnologyHirosaki UniversityHirosaki Aomori Japan;</p> <p>Department of Coupled Ocean‐Atmosphere-Land Processes Research (DCOP)Japan Agency for Marine‐Earth Science and Technology (JAMSTEC)Yokosuka Kanagawa Japan;</p> <p>Faculty of ScienceUniversity of the RyukyusNakakami‐gun Okinawa Japan;</p> <p>Climate and Ecosystems Dynamics Division Graduate School of BioresourcesMie UniversityTsu Mie Japan;</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=CMIP5&option=203" rel="nofollow">CMIP5;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=western equatorial Indian Ocean&option=203" rel="nofollow">western equatorial Indian Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SST bias&option=203" rel="nofollow">SST bias;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=heat budget analysis&option=203" rel="nofollow">heat budget analysis;</a> </p> <div class="translation"> 机译：CMIP5;西赤道印度洋;SST偏见;热预算分析; 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