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>Energetics of nonlinear internal waves generated by tidal flow over topography
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Energetics of nonlinear internal waves generated by tidal flow over topography
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机译:潮汐流在地形上产生的非线性内波的能量学
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An in-house fully nonlinear, nonhydrostatic numerical model is utilized for simulations of internal solitary waves (ISWs) generated by tidal flows over a Gaussian sill topography. A complete, rigorous theoretical framework is then adopted for the energetics analysis of these ISWs. The ratio of topographic amplitude to the total water depth is fixed, and the tidal excursion parameter (epsilon) and slope parameter (gamma) are varied by changing the imposed barotropic velocity and the horizontal scale of the topography. It is found that the energy input, conversion, and radiation rates all increase monotonically with epsilon. They peak when the bottom topography is critical (gamma - 1). The energy input is generated by the pressure difference across the domain. The energy conversion rate in percentage (normalized by the corresponding input rate) decreases almost linearly as epsilon increases. The larger the slope parameter, the higher the conversion percentage. The baroclinic radiation rate in percentage (normalized by the corresponding conversion rate) increases first and then decreases as e increases. It gets maximum near epsilon = 0.15, which corresponds to the emergence of ISWs in the flow field. The larger the slope parameter, the smaller the radiation percentage. At small epsilon value when the flow field is in the linear internal tide regime, the conversion and radiation percentages all agree very well with the results in existing literature (Kang and Fringer, 2012) for the Davidson Seamount. The barotropic and baroclinic dissipation percentages behave very differently. While the barotropic one is larger for smaller c, the baroclinic one is larger for larger gamma. The present work presents a relatively complete energy budget analysis of ISWs generated by tidal flow over a Gaussian sill topography. (C) 2013 Elsevier Ltd. All rights reserved.
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机译:内部的完全非线性,非静液压的数值模型用于模拟高斯门槛地形上的潮汐流产生的内部孤立波(ISW)。然后,采用完整,严格的理论框架对这些ISW进行能量学分析。地形振幅与总水深之比是固定的,潮汐偏移参数(ε)和坡度参数(γ)通过改变施加的正压速度和地形的水平比例而变化。发现能量输入,转换和辐射率都随ε单调增加。当底部地形非常关键时,它们达到峰值(伽玛-1)。能量输入是通过域上的压差产生的。随着ε的增加,以百分比表示的能量转换率(由相应的输入率标准化)几乎呈线性下降。斜率参数越大,转换百分比越高。斜压辐射率(以相应的转化率归一化)以百分比形式增加,然后随着e的增加而降低。它在ε= 0.15附近达到最大值,这对应于流场中ISW的出现。斜率参数越大,辐射百分比越小。当流场处于线性内潮态时,在小ε值下,转换和辐射百分率都与戴维森海山现有文献(Kang and Fringer,2012)中的结果非常吻合。正压和斜压耗散百分比的行为差异很大。对于较小的c,正压压力较大,而对于较大的γ,斜压压力较大。本工作提出了由高斯基台地形上的潮流产生的ISW的相对完整的能量收支分析。 (C)2013 Elsevier Ltd.保留所有权利。
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