Widespread Reemergence of Sea Surface Temperature Anomalies in the Global Oceans, Including Tropical Regions Forced by Reemerging Winds

Byju P.; Dommenget D.; Alexander M. A.

摘要

Abstract >Sea surface temperature anomalies (SSTA) in portions of the extratropics are known to recur from one winter to the next without persisting through the intervening summer. Previous studies identified only a limited number of midlatitude regions where this reemergence occurs. Here we find that most of the global oceans exhibit winter‐to‐winter recurrence of SSTA. Indeed, recurrence of SSTA is the default process in the global ocean. Only regions strongly linked to El Ni?o do not show signs of SST reemergence. In midlatitudes, the temperature anomalies that recur persist below the shallow mixed layer in summer. However, SST recurrence is also found at some tropical locations and appears to be independent of subsurface ocean heat storage. Reemergence at these locations is linked to the recurrence of atmospheric drivers of SSTA, predominantly the wind‐stress forcing. Our results are supported by different ocean data sets and by state‐of‐the‐art climate model simulations. </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>海表面温度异常（SSTA）中是已知的温带的部分，以从一个冬季复发到目前为止，不持续到临床夏天。以前的研究仅确定了这种重新调查的有限数量的中间地区。在这里，我们发现大多数全球海洋都展示了SSTA的冬季到冬季复发。实际上，SSTA的再次发生是全球海洋的默认过程。只有与El Ni强烈相关的地区才能显示SST综合性的迹象。在中期，在夏季，反复持续在浅层混合层下方的温度异常。然而，在一些热带地区也发现了SST复发，似乎与地下海洋蓄热的似乎无关。这些地点的综合性与SSTA的大气驱动程序的复发相关联，这主要是风力胁迫。我们的结果由不同的海洋数据集和最先进的气候模型模拟支持。</ p> </ abstract> </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>2018年第15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=Byju P.&option=202" target="_blank" rel="nofollow">Byju P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dommenget D.&option=202" target="_blank" rel="nofollow">Dommenget D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexander M. A.&option=202" target="_blank" rel="nofollow">Alexander M. A.;</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 Earth Atmosphere and EnvironmentMonash UniversityClayton Victoria Australia;</p> <p>School of Earth Atmosphere and EnvironmentMonash UniversityClayton Victoria Australia;</p> <p>NOAA/ESRLBoulder CO 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=sea surface temperature&option=203" rel="nofollow">sea surface temperature;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=winter‐to‐winter persistence&option=203" rel="nofollow">winter‐to‐winter persistence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean mixed layer&option=203" rel="nofollow">ocean mixed layer;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wind‐stress recurrence&option=203" rel="nofollow">wind‐stress recurrence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=CMIP models&option=203" rel="nofollow">CMIP models;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=weather and climate&option=203" rel="nofollow">weather and climate;</a> </p> <div class="translation"> 机译：海表面温度;冬季至冬季持久性;海洋混合层;风力复发;CMIP模型;天气和气候; </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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704019851816.html">Widespread Reemergence of Sea Surface Temperature Anomalies in the Global Oceans, Including Tropical Regions Forced by Reemerging Winds</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Byju P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Byju P.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dommenget D.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dommenget D.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexander M. A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alexander M. A. </a> <a href="/journal-foreign-23539/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geophysical Research Letters .</a> <span>2018</span><span>,第15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：全球海洋海面温度异常的广泛综述，包括通过再次风力迫使热带地区</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704013895610.html">Free and forced variability of the tropical Atlantic Ocean: role of the wind-evaporation-sea surface temperature feedback.</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mahajan S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mahajan S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Saravanan R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Saravanan R.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chang P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chang P. </a> <a href="/journal-foreign-33934/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Climate .</a> <span>2010</span><span>,第22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：热带大西洋的自由强迫变化：风蒸发海表面温度反馈的作用。</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070404205831.html">Variability in sea-surface temperature and winds in the tropical south-east Atlantic Ocean and regional rainfall relationships</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hermes JC&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hermes JC,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reason CJC&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Reason CJC </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>2009</span><span>,第1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：热带东南大西洋海洋表面温度和风的变化与区域降雨的关系</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_climate-change-conference-2013-impacts-policy-regulation_thesis/020512207968.html">Global Effects of Sea Surface Temperature Anomalies on Carbon Dioxide Exchange across the Atmosphere-Ocean Interface, 1996-2009</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Quinn J. Pallardy&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Quinn J. Pallardy,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thomas R. Marrero&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Thomas R. Marrero </a> <a href="/conference-foreign-33656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Climate Change Conference 2013: Impacts, Policy and Regulation .</a> <span>2013</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：海面温度异常对跨大气-海洋界面二氧化碳交换的全球影响，1996-2009年</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061646179.html">Mechanisms governing sea surface temperature anomalies in the eastern tropical Pacific Ocean associated with atmospheric intraseasonal variability</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lucas, Lisanne Elizabeth&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lucas, Lisanne Elizabeth </a> <span>2007</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：与大气季节内变化相关的东部热带太平洋海表温度异常的控制机制</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_detail_thesis/040002264958.html">Forced and unforced ocean temperature changes in Atlantic and Pacific tropical cyclogenesis regions</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=B. D. Santer&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">B. D. Santer,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. M. L. Wigley&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. M. L. Wigley,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P. J. Gleckler&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">P. J. Gleckler,</a> <span>2006</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：大西洋和太平洋热带气旋作用区域的强迫和非强迫海洋温度变化</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100022770768.html ">The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content.</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McGregor, Helen V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">McGregor, Helen V.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Evans, Michael N.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Evans, Michael N.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Goosse, Hugues&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Goosse, Hugues,</a> <span>2015</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：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_pb_thesis/020711288483.html">Atlantic Oceanographic and Meteorological Laboratory Fiscal Year 1983 Annual Report. El Nino: June 1983 Surface Temperature Anomalies (Degrees C) in the Tropical Pacific Ocean</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> </a> <span>1983</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：大西洋海洋学和气象实验室1983财年年度报告。厄尔尼诺：1983年6月热带太平洋地表温度异常（C级）</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130430379802.html">ELECTRON-INTERFERENCE METHOD OF DETECTING LOCATION AND TYPES OF MOLECULAR GROUPS ON SURFACES OF SMALL BIO OBJECTS INCLUDING NUCLEOTIDE SEQUENCES AND DEVICE THEREFOR(57) The invention relates to detecting a bio-objects structure, it can be used in studying surface structure of small bio-objects such as macromolecules and detecting a location and a type of molecular groups disposed thereon. A device comprises a base with a substrate made from a non-conductive material thereon, a photocathode and an anode, wherein there is a site therebetween for an object to be studied and electron scatterers. There is at least one window inside the photocathode, the photocathode areas bordering the window made from a material with a reduced work function. The window is connected to a region beyond the photocathode by at least one slit, its length exceeds its width. A cooling electrode is arranged at a small depth under the window and the slit region, wherein an accelerating electrode is arranged the ph</a> <b>[P]</b> . <span> 外国专利：  EA012215B1 </span> <span> . 2009-08-28</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：检测包括核苷酸序列和装置在内的小生物物体表面上分子组的位置和类型的电子干扰方法（57）本发明涉及检测生物物体的结构，可用于研究小型生物物体的表面结构物体（例如大分子）并检测其上放置的分子的位置和类型。一种装置，包括具有在其上的由非导电材料制成的基底的基底，光电阴极和阳极，其中在其之间存在用于研究对象的位置和电子散射体。光电阴极内至少有一个窗口，该光电阴极区域与窗口相邻，该窗口由功函数降低的材料制成。窗口通过至少一个狭缝连接到光电阴极之外的区域，其长度超过其宽度。在窗口和狭缝区域下方以较小的深度布置有冷却电极，其中在电极和缝隙区域下方布置有加速电极。 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130404585547.html">System and method for correcting a model-derived vertical structure of ocean temperature and ocean salinity based on sea surface height observations</a> <b>[P]</b> . <span> 外国专利：  US10268783B2 </span> <span> . 2019-04-23</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：基于海面高度观测的校正模型推导的海洋温度和盐度垂直结构的系统和方法 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130412778309.html">SYSTEM AND METHOD FOR CORRECTING A MODEL-DERIVED VERTICAL STRUCTURE OF OCEAN TEMPERATURE AND OCEAN SALINITY BASED ON SEA SURFACE HEIGHT OBSERVATIONS</a> <b>[P]</b> . <span> 外国专利：  US2016117423A1 </span> <span> . 2016-04-28</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：基于海面高度观测的海洋温度和海洋盐度模型源垂直结构校正系统和方法 </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 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