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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Spatial Distribution of Diffusivity Coefficients and the Effects on Water Mass Modification in the North Pacific
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Spatial Distribution of Diffusivity Coefficients and the Effects on Water Mass Modification in the North Pacific

机译:扩散系数的空间分布及对北太平洋水质改性的影响

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Abstract >Three‐dimensional velocity, diapycnal mixing, and isopycnal mixing fields were estimated based on long‐term mean (2001–2015) salinity distributions obtained with Argo float arrays on neutral‐density (γ) surfaces. Strong estimated isopycnal mixings were associated with the Kuroshio Extension, subtropical boundary, and the west coast of North America, and strong estimated diapycnal mixing was associated with the Izu‐Ogasawara and Hawaiian ridges, which are internal wave‐generation spots. Patterns of the mixing coefficient distributions were consistent with previous estimates by other methods. We used the mixing coefficient fields to reveal the spatial patterns of volume transports and salinity budgets on isopycnal layers. Whereas relatively large eddy transports associated with thickness diffusivity contributed to the spatial patterns of volume transports, the contributions of spatial changes in diapycnal mixing were small. Spatial changes of diapycnal mixing strongly affected those of salinity, especially in the layers around North Pacific Intermediate Water (26.5–27.0γ and 27.0–27.5γ), whereas spatial changes of isopycnal mixing were important for water mass modification in all layers. This analysis suggests that the clear salinity minimum formed regionally along the Kuroshio Extension decays because of locally strong diapycnal mixing as well as isopycnal mixing. Although the results support the utility of using the spatial distributions of water properties to infer water mass modifications, assessments based on direct measurements of mixing and fine‐scale parameterization are needed to clarify the localized effects of mixing on water mass modifications because the inversion errors in this study were not small enough to enable detection of high‐resolution spatial changes. </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> >三维速度,基于长期平均值(2001-2015)盐度估计了三维速度,二进曲混合和等离子体混合场用Argo浮子阵列获得的中性密度(γ)表面获得的分布。强大的估计等离子体混合与Kuroshio延伸,亚热带边界和北美西海岸有关,强烈估计的十几个混合与Izu-ogasawara和夏威夷脊有关,这是内部波浪发射斑点。混合系数分布的图案与其他方法的先前估计一致。我们利用混合系数域来揭示异维层上的体积传输和盐度预算的空间模式。然而,与厚度扩散率相关联的相对较大的涡流运输导致体积传输的空间模式,但延迟混合中的空间变化的贡献很小。二尾搅拌的空间变化强烈影响盐度,特别是在北太平洋中间水(26.5-27.0γ和27.0-27.5〜)周围的层中,而等素混合的空间变化对于所有层中的水质改性是重要的。该分析表明,由于局部强劲的十进性混合以及异构菌混合,沿着Kuroshio延伸衰减地区形成的透明盐度最小。虽然结果支持使用水性空间分布的效用来推断水质量修改,但需要基于混合和微尺度参数化的直接测量的评估,以阐明混合在水质量修改上的局部效果,因为反转误差该研究不足以使能够检测高分辨率空间变化。</ 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15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=Kouketsu Shinya&option=202" target="_blank" rel="nofollow">Kouketsu Shinya;</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>Japan Agency for Marine‐Earth Science and Technology (JAMSTEC)Yokosuka 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=water mass modification&option=203" rel="nofollow">water mass modification;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=NPIW&option=203" rel="nofollow">NPIW;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=isopycnal mixing&option=203" rel="nofollow">isopycnal mixing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=diapycnal mixing&option=203" rel="nofollow">diapycnal mixing;</a> </p> <div class="translation"> 机译:水质量修饰;NPIW;异构菌混合;十进月的混合; </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/0704025580329.html">Spatial Distribution of Diffusivity Coefficients and the Effects on Water Mass Modification in the North Pacific</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kouketsu Shinya&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kouketsu Shinya </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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