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A Modeling Study of Interannual Variability of Bay of Bengal Mixing and Barrier Layer Formation

机译:孟加拉混合湾持续变异性的建模研究

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Abstract > The year to year variability of surface mixing in the Bay of Bengal (BoB) is examined with the help of an Ocean Dynamic‐Thermodynamic Model (ODTM) and observational data. The model embeds a conventional nonlinear primitive equation based reduced gravity model (RGM) with “N” active layers overlying a 1/2 quiescent layer. The model is coupled to a high‐resolution mixed layer model (MLM) to capture the physics of the mixed layer. The MLM incorporates a level‐2 turbulence closure mixing scheme based on Mellor and Yamada (1982). As a result of the coupling, our model calculates the net hydrostatic pressure as a sum of those due to the thickness of RGM layers with constant densities and due to the dynamic topography of MLM levels with variable densities. At each time step the coupling between RGM and MLM is achieved as follows: (i) a layer‐averaged tendency of momentum and tracers (i.e., temperature and salinity) of the MLM is updated to the RGM, (ii) momentum and tracers of the MLM get advected by large‐scale horizontal dynamics of the RGM, and (iii) horizontal layer divergence of the RGM aides for the vertical advection of the MLM. By virtue of this coupling, the model faithfully reproduces the seasonal cycle of temperature, salinity, sea surface height, thermocline, mixed and barrier layer thickness of the tropical Indian Ocean. A simulation with Coordinated Ocean‐Ice Reference Experiment (CORE) forcing for 15 years (from 1995 to 2009) is used as a test case to study the interannual variability (IAV) of the mixed layer depth and barrier layer thickness (BL) in BoB. The dominant modes of IAV in the BoB mixing are governed by the correspondingly varying surface momentum, heat, and fresh water fluxes with very little contribution from entrainment of heat and/or salt at the base of the mixed layer. Further, these fluxes are controlled by El Ni?o‐Southern Oscillation (ENSO) varia </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”>抽象</ title> >在海洋动态的帮助下,检查了孟加拉湾(BOB)的表面混合的年度变异性的年份热力学模型(ODTM)和观测数据。该模型将传统的非线性原始方程基于覆盖1/2静止层的“n”有源层的常规非线性原始方程基于缩小的重力模型(RGM)。该模型耦合到高分辨率混合层模型(MLM)以捕获混合层的物理学。 MLM采用基于MELLOR和YAMADA(1982)的水平-2湍流闭合混合方案。由于耦合,我们的模型将净水压压力计算为具有恒定密度的RGM层的厚度,并且由于具有可变密度的MLM水平的动态形貌,因此是由于RGM层的厚度。在每个时间步骤中,如下实现RGM和MLM之间的耦合:(i)将MLM的动量和示踪剂(即,温度和盐度)的层平均趋势更新为RGM,(II)动量和示踪剂MLM通过RGM的大规模水平动态进行,(III)RGM助手的水平层分歧,用于MLM的垂直平流。凭借这种耦合,该模型忠实地再现了热带印度洋的温度,盐度,海表面高度,热控,混合和阻挡层厚度的季节性循环。具有协调的海洋冰参考实验(核心)迫使15年(1995年至2009年)的模拟用作研究鲍勃中混合层深度和阻挡层厚度(BL)的依赖性变异性(IAV)的测试案例。鲍勃混合中IAV的显性模式受相应变化的表面动量,热量和淡水通量的管辖,从混合层的底部夹带加热和/或盐的夹带而具有非常小的贡献。此外,这些助熔剂由El Niα→O-南部振荡(ENSO)Varia控制 </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20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=Valsala Vinu&option=202" target="_blank" rel="nofollow">Valsala Vinu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Singh Shikha&option=202" target="_blank" rel="nofollow">Singh Shikha;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Balasubramanian Sridhar&option=202" target="_blank" rel="nofollow">Balasubramanian Sridhar;</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>Training Center Indian Institute of Tropical MeteorologyPune India;</p> <p>Training Center Indian Institute of Tropical MeteorologyPune India;</p> <p>Interdisciplinary Programme in Climate Studies Indian Institute of TechnologyBombay India;</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=Bay of Bengal&option=203" rel="nofollow">Bay of Bengal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mixed layer depth&option=203" rel="nofollow">mixed layer depth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=barrier layer depth&option=203" rel="nofollow">barrier layer depth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean modeling&option=203" rel="nofollow">ocean modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=turbulent closure model&option=203" rel="nofollow">turbulent closure model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=interannual variability of mixing&option=203" rel="nofollow">interannual variability of mixing;</a> </p> <div class="translation"> 机译:孟加拉湾;混合层深度;屏障层深度;海洋建模;湍流闭合模型;混合的续变性; </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/0704025580679.html">A Modeling Study of Interannual Variability of Bay of Bengal Mixing and Barrier Layer Formation</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Valsala Vinu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Valsala Vinu,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Singh Shikha&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Singh Shikha,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Balasubramanian Sridhar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Balasubramanian Sridhar </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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href="/patent-detail/061202016163.html">评估设计参数变异性对混合料动态模量变异性影响的方法</a> <b>[P]</b> . <span> 中国专利: CN104614508B </span> <span> . 2016.04.13</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120107135314.html">评估设计参数变异性对混合料动态模量变异性影响的方法</a> <b>[P]</b> . <span> 中国专利: CN104614508A </span> <span> . 2015-05-13</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130492354019.html">a layered material for models used to study the metal during plastic deformation, and the method of its manufacture</a> <b>[P]</b> . <span> 外国专利: <!-- --> SU103094A1 </span> <span> . 1955-11-30</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:用于研究塑性变形过程中金属的模型的分层材料及其制造方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130449402146.html">BAYESIAN INFERENCE METHOD FOR MIXED 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