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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Eastward propagating decadal temperature variability in the SS outh AA tlantic and II ndian OO ceans
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Eastward propagating decadal temperature variability in the SS outh AA tlantic and II ndian OO ceans

机译：东方传播二等温度变异 s s Outh. a a Tlantic和 i i NDian. O o 芯片

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Abstract > The origin and structure of eastward propagating decadal temperature variability in the South Atlantic and Indian Oceans are investigated by using long‐term output of coupled general circulation model. Composite analysis during the warm Southwest Indian Ocean (SWIO) years shows that decadal temperature anomalies in the SWIO region originate in the South Atlantic and are associated with density anomalies. Since the density anomalies propagate at the speed of a few cm s ?1 , slower than the speed of the background eastward Antarctic Circumpolar Current, and exhibit a surface‐intensified equivalent barotropic structure, the eastward propagation of the density anomalies may be attributed to quasi‐stationary oceanic Rossby waves. The density anomalies are also accompanied with anomalous Ekman pumping, indicating an important contribution from the overlying atmospheric variability. The role of atmospheric variability is further examined by evaluating the mixed‐layer heat balance. It is found that the warm temperature anomalies in the South Atlantic are due to anomalous entrainment and meridional advection. These results suggest that the atmospheric variability plays an important role through the ocean mixed layer in generating the eastward propagation of decadal temperature variability from the South Atlantic besides the internal ocean variability as suggested in previous studies. </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> > 利用耦合通用循环模型的长期输出，研究了南大西洋和印度洋的东部传播二等温度变异性的起源和结构。温暖西南印度洋（SWIO）多年来的综合分析表明，SWIO区域的二等温度异常源于南大西洋，与密度异常相关。由于密度异常以几厘米的速度传播 ？1 </ sup> ，比背部南极环形电流的速度慢，表现出表面强化的等效波调结构，密度异常的东方传播可能归因于准静止海洋rossby波。密度异常也伴随着异常的EKMAN泵送，表明来自覆盖大气变异性的重要贡献。通过评估混合层热平衡进一步检查大气变异性的作用。发现南部大西洋的温暖温度异常是由于异常的夹带和优势平流。这些结果表明，除了在先前研究中提出的内部海洋变异之外，大气变异性通过海洋混合层通过海洋混合层发挥着重要作用。 </ 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7期</span><b style="margin: 0 2px;">|</b><span>共13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=Morioka Yushi&option=202" target="_blank" rel="nofollow">Morioka Yushi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Taguchi Bunmei&option=202" target="_blank" rel="nofollow">Taguchi Bunmei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Behera Swadhin K.&option=202" target="_blank" rel="nofollow">Behera Swadhin K.;</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>Application LaboratoryJAMSTECYokohama Japan;</p> <p>Application LaboratoryJAMSTECYokohama Japan;</p> <p>Application LaboratoryJAMSTECYokohama 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=decadal temperature variability&option=203" rel="nofollow">decadal temperature variability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South Atlantic&option=203" rel="nofollow">South Atlantic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Southern Indian Ocean&option=203" rel="nofollow">Southern Indian Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eastward propagation&option=203" rel="nofollow">eastward propagation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic Rossby waves&option=203" rel="nofollow">oceanic Rossby waves;</a> </p> <div class="translation"> 机译：十二次温度变异;南大西洋;南印度洋;东方传播;海洋罗斯比波浪; </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/0704025580716.html">Eastward propagating decadal temperature variability in the <fc xmlns="http://www.wiley.com/namespaces/wiley">S</fc>S outh <fc xmlns="http://www.wiley.com/namespaces/wiley">A</fc>A tlantic and <fc xmlns="http://www.wiley.com/namespaces/wiley">I</fc>I ndian <fc xmlns="http://www.wiley.com/namespaces/wiley">O</fc>O ceans</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Morioka Yushi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Morioka Yushi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Taguchi Bunmei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Taguchi Bunmei,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Behera Swadhin K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Behera Swadhin K. </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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