2010
DOI: 10.1007/s10665-010-9388-6
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The uniform asymptotic form of the internal gravity-wave field generated by a source moving above a smoothly varying bottom

Abstract: The uniform asymptotic form of the internal gravity-wave field generated by a source moving above a smoothly varying bottom is constructed. The problem of reconstructing non-harmonic internal gravity-wave packets generated by a source moving in a stratified ocean is considered. The solution is proposed in terms of wave modes, propagating independently at the adiabatic approximation, and described as a non-integral-degree series of a small parameter characterizing the stratified medium. A specific form of the w… Show more

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Cited by 10 publications
(19 citation statements)
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“…where L is the typical scale of the horizontal variations 0 ρ , h is the typical scale of the vertical variations 0 ρ (for example, the thermocline width) [13,15]. In non-dimension coordinates the equation system (2) will be written as (index * is omitted hereafter)…”
Section: Asymptotical Analysis Of Internal Gravity Wave Dynamics 221mentioning
confidence: 99%
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“…where L is the typical scale of the horizontal variations 0 ρ , h is the typical scale of the vertical variations 0 ρ (for example, the thermocline width) [13,15]. In non-dimension coordinates the equation system (2) will be written as (index * is omitted hereafter)…”
Section: Asymptotical Analysis Of Internal Gravity Wave Dynamics 221mentioning
confidence: 99%
“…, which are assumed to be known [15] . From here on the index n will be omitted while assuming that further calculations belong to an individually taken mode.…”
Section: Asymptotic Solutionsmentioning
confidence: 99%
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“…The present issue is concerned with body motion in a two-layer fluid [6], interaction of water waves with a porous plate [7], displacement of one fluid by another in a porous medium [8], liquid-film flows over a step topography with external electric field [9], turbulent flows produced on rotating blades [10], a water-impact problem [11], the Maslov canonical operator for shallow-water equations with localized initial data [12], internal gravity waves over a bottom topography [13], a reaction-diffusion model for concrete corrosion in sewer pipes [14] and convection in a two-layer fluid with external high-frequency vibration [15]. Different methods of asymptotic analysis such as the homogenization method, the Maslov canonical operator, the method of matched asymptotic expansions, generalized methods from geometric optics, and their combinations with numerical methods are used to demonstrate their practical importance in the analysis of practical problems.…”
mentioning
confidence: 99%