Spreading of the South Pacific Tropical Water and Antarctic Intermediate Water Over the Maritime Continent

Yang Lina; Zhou Lei; Li Shujiang; Wei Zexun

摘要

Abstract >The three‐dimensional climatological spreading of South Pacific waters over the Maritime Continent is examined using eddy‐resolving simulations and a passive tracer method. Four pathways are summarized for the South Pacific Tropical Water and the Antarctic Intermediate Water through the Maritime Continent, including two direct pathways, namely, the Eastern Path and the Torres Strait Path, and two indirect pathways, namely, the Western Path and the South China Sea Path. Among them, according to tracer concentration distribution, the former two contribute most of the volume transport of the Indonesian Throughflow (ITF) originating from the South Pacific. The latter two experience two retroflections (i.e., the South Equatorial Current‐Equatorial Undercurrent and the North Equatorial Countercurrent‐North Equatorial Current) before entering the Indonesian Seas. The vertical distributions of the South Pacific waters along each path throughout the Indonesian Seas are also analyzed, revealing that the South Pacific salinity extrema greatly affect the intermediate and deep layers of the Indonesian Seas and ITF as well as the upper thermocline. Vertical fluxes, especially vertical advection, are vital to these Indo‐Pacific water exchange processes. Sensitivity tests are conducted for the vertical diffusion coefficient and initial conditions, the results of which are robust. According to current study, the South Pacific has substantial impacts on the water properties throughout the Maritime Continent and the mass‐energy exchanges between the Pacific and Indian Oceans. </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”>摘要</ title> >使用涡流模拟和被动示踪方法检查南太平洋水域对海洋大陆的三维气候蔓延。南太平洋热带水和南极中间水总结了四条途径，包括两个直接途径，即东部路径和托雷斯海峡路径，以及两条间接途径，即西部道路和华南地区海道路。其中，根据示踪剂浓度分布，前两者有助于源自南太平洋的印度尼西亚通风流量（ITF）的大部分体积运输。在进入印度尼西亚海洋之前，后两者经历了两次重新回形（即，南赤道电流赤道暗流和北赤道逆流 - 北赤道电流）。还分析了南太平洋水域沿着印度尼西亚海洋的各道路的垂直分布，揭示了南太平洋盐度极值极大地影响印度尼西亚海洋和ITF的中间和深层以及上层热水管制。垂直助焊剂，特别是垂直平流，对这些印度水交换过程至关重要。对垂直扩散系数和初始条件进行敏感性测试，其结果是稳健的。根据目前的研究，南太平洋对整个海洋大陆的水质和太平洋和印度洋之间的大规模能源交流产生了重大影响。</ 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-34643/'>《Journal of Geophysical Research, C. Oceans: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第6期</span><b style="margin: 0 2px;">|</b><span>共24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=Yang Lina&option=202" target="_blank" rel="nofollow">Yang Lina;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhou Lei&option=202" target="_blank" rel="nofollow">Zhou Lei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Shujiang&option=202" target="_blank" rel="nofollow">Li Shujiang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei Zexun&option=202" target="_blank" rel="nofollow">Wei Zexun;</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 Marine Science and Numerical ModelingFirst Institute of Oceanography State Oceanic AdministrationQingdao China;</p> <p>Institute of OceanographyShanghai Jiao Tong UniversityShanghai China;</p> <p>Key Laboratory of Marine Science and Numerical ModelingFirst Institute of Oceanography State Oceanic AdministrationQingdao China;</p> <p>Key Laboratory of Marine Science and Numerical ModelingFirst Institute of Oceanography State Oceanic AdministrationQingdao 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=Indonesian Throughflow&option=203" rel="nofollow">Indonesian Throughflow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South Pacific Tropical Water&option=203" rel="nofollow">South Pacific Tropical Water;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Antarctic Intermediate Water&option=203" rel="nofollow">Antarctic Intermediate Water;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=passive tracers&option=203" rel="nofollow">passive tracers;</a> </p> <div class="translation"> 机译：印度尼西亚通过流量;南太平洋热带水;南极中间水;被动示踪剂; </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/0704025579377.html">Spreading of the South Pacific Tropical Water and Antarctic Intermediate Water Over the Maritime Continent</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Lina&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yang Lina,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhou Lei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhou Lei,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Shujiang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Shujiang,</a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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Berelson,</a> <span>2016</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：从封面开始：热带东太平洋南太平洋地表水固氮率低</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000124120306.html">Spreading of the South Pacific Tropical Water and Antarctic Intermediate Water Over the Maritime Continent</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lina Yang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lina Yang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lei Zhou&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lei Zhou,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shujiang Li&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shujiang Li,</a> <span>2018</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：在海洋大陆的南太平洋热带水和南极中间水的传播</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-ocean-university-china-natural-science-edition_thesis/0201298352125.html">“Tasman”海中的南太平洋副热带模态水</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=胡海波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 胡海波</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘秦玉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘秦玉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=林霄沛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,林霄沛</a> <span> <a href="/journal-cn-50383/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国海洋大学学报：自然科学版 </a> </span> <span> . 2007</span><span>,第2期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_marine-sciences_thesis/0201253849799.html">北太平洋副热带中部模态水潜沉区的热收支⎯⎯一个全球海洋模式数据的结果</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=聂珣炜&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 聂珣炜</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高山&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,高山</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王凡&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王凡</a> <span> <a href="/journal-cn-4975/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋科学 </a> </span> <span> . 2013</span><span>,第009期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-human-environment_thesis/0201269214813.html">逆转流动：使海洋的水和养分流向大陆</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hode.CN&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . Hode.CN</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=沈晶&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,沈晶</a> <span> <a href="/journal-cn-53666/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 人类环境杂志 </a> </span> <span> . 1993</span><span>,第007期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-oceanologica-sinica_thesis/0201253882442.html">西北太平洋副热带模态水形成区声传播特性分析</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张旭&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张旭</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=程琛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,程琛</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘艳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘艳</a> <span> <a href="/journal-cn-4977/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋学报（中文版） </a> </span> <span> . 2014</span><span>,第009期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-polar-research_thesis/0201253928697.html">南极普里兹湾海域夏季表层水与绕极深层水年际变化</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴成祥&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 吴成祥</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李丙瑞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李丙瑞</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=左菲&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,左菲</a> <span> <a href="/journal-cn-4982/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 极地研究 </a> </span> <span> . 2017</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-24671_thesis/020221198564.html">塔斯曼海中南太平洋副热带模态水的特征</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=胡海波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 胡海波</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘秦玉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘秦玉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=林霄沛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,林霄沛</a> <span> <a href="/conference-cn-24671/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国首届Argo科学研讨会 </a> <span> <span> . 2006</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314992610.html">热带东印度洋上层海洋环流及其与孟加拉湾水交换的季节变化研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=宣莉莉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 宣莉莉</a> <span> . 2013</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061202325310.html">水酶法制备南极磷虾油及其微胶囊和低氟南极磷虾肽的方法</a> <b>[P]</b> . <span> 中国专利： CN104388176B </span> <span> . 2017.01.25</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120103068325.html">水酶法制备南极磷虾油及其微胶囊和低氟南极磷虾肽的方法</a> <b>[P]</b> . <span> 中国专利： CN104388176A </span> <span> . 2015-03-04</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130400966046.html">The SMA -Eden BM3 (EDEN3) is an extension of the Snowy Mountains Hydro Scheme. The purpose of this engineering project is to safeguard regions of south-eastern Australia now, and in the future, from drought and to supply water as climate change impacts. The EDEN3 will supply de-salinated water from the NSW South Coast and pump it up near the Brown Mountain area into the Murrumbidgee River. This water will flow to Lake Burrinjuck and then be piped into Lake George and into the Shoalhaven River. It is designed to provide a secure water supply to the Eden-Monaro area and provide power.</a> <b>[P]</b> . <span> 外国专利：  AU2020100956A4 </span> <span> . 2020-08-06</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：SMA-Eden BM3（EDEN3）是雪山水电计划的扩展。该工程项目的目的是保护澳大利亚东南部的地区现在以及将来免受气候变化影响的干旱和供水。 EDEN3将从新南威尔士州南海岸供应淡化水，并将其泵入布朗山区附近，进入穆伦比吉河。这些水将流向Burrinjuck湖，然后通过管道输送到George湖和Shoalhaven河。它旨在为Eden-Monaro地区提供安全的水并提供电力。 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130417736020.html">Use of particles of a Water Absorbing insoluble Dietary ingredient as a carrier for Water and / or a Moisturizer, because it serves to water entering a tropicalization chocolate product; agent; chocolate Product tropicalized, method for the preparation of the AG Body; and a method to improve the heat stability</a> <b>[P]</b> . <span> 外国专利：  CL2014000762A1 </span> <span> . 2014-08-29</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：使用吸水不溶性膳食成分的颗粒作为水和/或保湿剂的载体，因为它可以使水进入热带巧克力产品;代理商热带化的巧克力产品，AG主体的制备方法;和改善热稳定性的方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130439099069.html">Marine photo-bioreactor for production of phototropic organisms in tropical or sub-tropical waters</a> <b>[P]</b> . <span> 外国专利：  DE10322111A1 </span> <span> . 2004-12-02</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：海洋光生物反应器，用于在热带或亚热带水域生产光致生物 </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> 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