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Energy Spectrum of Linear Internal Wave Field in the Vicinity of Continental Slope

Energy Spectrum of Linear Internal Wave Field in the Vicinity of Continental Slope
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摘要 The purpose of the research was to investigate two-dimensional modeling of efficiency of mixing, resulting from the reflection of a linear internal wave field (IWF) off a continental slope. Efficiency of deep ocean mixing was associated with the energy balance of the radiating IWF into an interior of the ocean in the vicinity of a sloping bottom topography. Since waves are generated not only at the fundamental frequency but also at all of its harmonics <em>ω</em><sub><em>n</em></sub> = <em>nω</em> less than buoyancy frequency <i>N</i> and greater than Coriolis frequency <i>f</i>, our analysis includes, in general, an infinite number of discrete internal wave modes <i>n</i> satisfying the dispersion relationship for internal waves. However, since we are interested only in the radiating part of the field, the mode numbers are limited. Due to multiple singularities of order two caused by resonance in the vicinity of critical slope, the energy is visualized in <em>L</em><sub><em>δ</em></sub> -norm with <em>δ</em> > 2. Research results include the visualization of the effects of the continental slope and the Earth’s rotation on resulting energy in the vicinity of the slope. The purpose of the research was to investigate two-dimensional modeling of efficiency of mixing, resulting from the reflection of a linear internal wave field (IWF) off a continental slope. Efficiency of deep ocean mixing was associated with the energy balance of the radiating IWF into an interior of the ocean in the vicinity of a sloping bottom topography. Since waves are generated not only at the fundamental frequency but also at all of its harmonics <em>ω</em><sub><em>n</em></sub> = <em>nω</em> less than buoyancy frequency <i>N</i> and greater than Coriolis frequency <i>f</i>, our analysis includes, in general, an infinite number of discrete internal wave modes <i>n</i> satisfying the dispersion relationship for internal waves. However, since we are interested only in the radiating part of the field, the mode numbers are limited. Due to multiple singularities of order two caused by resonance in the vicinity of critical slope, the energy is visualized in <em>L</em><sub><em>δ</em></sub> -norm with <em>δ</em> > 2. Research results include the visualization of the effects of the continental slope and the Earth’s rotation on resulting energy in the vicinity of the slope.
作者 Ranis N. Ibragimov Austin Biondi Nathan Arndt Maria Castillo Guang Lin Vesselin Vatchev Sheng Zhang Ranis N. Ibragimov;Austin Biondi;Nathan Arndt;Maria Castillo;Guang Lin;Vesselin Vatchev;Sheng Zhang(Wenatchee Valley College, Wenatchee, WA, USA;University of Wisconsin-Parkside, Kenosha, WI, USA;Purdue University, West Lafayette, IN, USA;University of Texas Rio Grande, Edinburg, TX, USA)
出处 《Journal of Applied Mathematics and Physics》 2020年第10期2256-2274,共19页 应用数学与应用物理(英文)
关键词 Internal Wave Field Effects of Rotation Continental Slope Energy Radiation Internal Wave Field Effects of Rotation Continental Slope Energy Radiation
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