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Wind Power on Oceanic Near‐Inertial Oscillations in the Global Ocean Estimated From Surface Drifters

机译：全球海洋近惯性振荡的风力估算从表面漂移者估算

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Abstract >Wind power on oceanic near‐inertial oscillations is thought to play an important role in furnishing the diapycnal mixing in the ocean. Yet their global distribution and magnitude have not been quantified based on observations. In this study, we use hourly ocean current records derived from surface drifters to compute the global near‐inertial wind power during 1993–2016, with a combination of surface wind measurements obtained from satellites. The climatological near‐inertial wind power integrated between 60°S and 60°N is estimated to be 0.3–0.6?TW. The strongest energy flux occurs in the 30–60° latitude band during the winter season as a result of energetic storm activities. Ocean current imprint on wind stress has a significant impact on the estimated global near‐inertial wind power from drifters. Neglecting this imprint overestimates the near‐inertial wind power locally by 25–120% and its global mean value by 60%. </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”xml：lang =“en”> <title type =“main”>抽象</ title> >风力对海洋附近惯性振荡的风电被认为在提供十腹的循环中发挥重要作用在海洋中混合。然而，他们的全球分布和幅度尚未根据观察定量量化。在这项研究中，我们使用从表面漂移器中得出的每小时海洋电流记录，以在1993 - 2016年期间计算全球近惯风电力，具有从卫星获得的表面风测量的组合。集成在60°S和60°N之间的气候近惯性风力估计为0.3-0.6。由于精力充沛的风暴活动，冬季的30-60°纬度带发生了最强的能量通量。风力应力的海洋电流印记对来自漂移者的估计全球近乎惯性风力产生重大影响。忽略该印记高估了25-120％局部近惯性风力，其全球平均值达到60％。</ 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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2019年第5期</span><b style="margin: 0 2px;">|</b><span>共7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=Liu Yongzheng&option=202" target="_blank" rel="nofollow">Liu Yongzheng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jing Zhao&option=202" target="_blank" rel="nofollow">Jing Zhao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu Lixin&option=202" target="_blank" rel="nofollow">Wu Lixin;</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 Physical Oceanography/Institute for Advanced Ocean StudiesOcean University of China and Qingdao National Laboratory for Marine Science and TechnologyQingdao China;</p> <p>Key Laboratory of Physical Oceanography/Institute for Advanced Ocean StudiesOcean University of China and Qingdao National Laboratory for Marine Science and TechnologyQingdao China;</p> <p>Key Laboratory of Physical Oceanography/Institute for Advanced Ocean StudiesOcean University of China and Qingdao National Laboratory for Marine Science and TechnologyQingdao China;</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=near‐inertial oscillations&option=203" rel="nofollow">near‐inertial oscillations;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wind power&option=203" rel="nofollow">wind power;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=global drifter program&option=203" rel="nofollow">global drifter program;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=CCMP&option=203" rel="nofollow">CCMP;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=buoy&option=203" rel="nofollow">buoy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=observation&option=203" rel="nofollow">observation;</a> </p> <div class="translation"> 机译：近惯性振荡;风力;全球漂移程序;CCMP;浮标;观察; </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/0704019852295.html">Wind Power on Oceanic Near‐Inertial Oscillations in the Global Ocean Estimated From Surface Drifters</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Yongzheng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Liu Yongzheng,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jing Zhao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jing Zhao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu Lixin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wu Lixin </a> <a href="/journal-foreign-23539/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geophysical Research Letters .</a> <span>2019</span><span>,第5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：全球海洋近惯性振荡的风力估算从表面漂移者估算</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704014398352.html">Global ocean surface velocities from drifters: Mean, variance, El Ni?o-Southern Oscillation response, and seasonal cycle</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lumpkin R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lumpkin R.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Johnson G.C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Johnson G.C. </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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Felicísimo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ángel M. Felicísimo,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jesús Muñoz&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jesús Muñoz,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jacob González-Solis&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jacob González-Solis </a> <span>2008</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：海洋表面风驱动跨洋空中运动的动力学</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/020711235381.html">Relationships between Surface Observations over the Global Oceans and the Southern Oscillation</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wright, P. B. &option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wright, P. B. ,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mitchell, T. P. &option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mitchell, T. P. ,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wallace, J. M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wallace, J. M. </a> <span>1985</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：全球海洋地表观测与南方涛动的关系</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-ocean-technology_thesis/0201221673222.html">近实时全球海洋表层流场估算方法研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙鹤泉1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙鹤泉1</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周虹丽2&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,周虹丽2</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张志刚1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张志刚1</a> <span> <a href="/journal-cn-23101/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋技术学报 </a> </span> <span> . 2015</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-ocean-technology_thesis/0201253814890.html">近实时全球海洋表层流场估算方法研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙鹤泉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙鹤泉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周虹丽&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,周虹丽</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张志刚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张志刚</a> <span> <a href="/journal-cn-4973/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋技术 </a> </span> <span> . 2015</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-tropical-oceanography_thesis/0201252194659.html">利用温度剖面资料结合海面高度估算全球海洋上层热含量异常</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘增宏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘增宏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许建平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,许建平</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙朝辉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,孙朝辉</a> <span> <a href="/journal-cn-4810/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 热带海洋学报 </a> </span> <span> . 2013</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-tropical-oceanography_thesis/0201252198289.html">全球海洋与大气界面的熵通量估算</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=严幼芳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 严幼芳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=甘子钧&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,甘子钧</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=齐义泉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,齐义泉</a> <span> <a href="/journal-cn-4810/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 热带海洋学报 </a> </span> <span> . 2004</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-oceanologica-sinica_thesis/0201293011151.html">基于船载无人机的绿潮漂移速度估算与分析</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=姜晓鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 姜晓鹏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高志强&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,高志强</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴晓青&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吴晓青</a> <span> <a href="/journal-cn-50857/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋学报 </a> </span> <span> . 2021</span><span>,第4期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-6100_thesis/020221602146.html">利用温度剖面资料结合海面高度估算全球海洋上层热含量异常</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LIU Zenghong&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . LIU Zenghong</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘增宏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘增宏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=XU Jianping&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,XU Jianping</a> <span> <a href="/conference-cn-6100/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第八届全国海洋资料同化研讨会暨第二届Argo科学研讨会 </a> <span> <span> . 2013</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020316087049.html">习惯性与非习惯性情绪调节对估算策略执行的影响</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=胡胜杰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 胡胜杰</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" 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