2011
DOI: 10.1098/rspa.2011.0193
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Generation of internal gravity waves by an oscillating horizontal disc

Abstract: Internal gravity waves are generated in a stratified fluid by arbitrary forced oscillations of a horizontal disc. The wave fields are calculated in both the time domain and the frequency domain. In the time domain, an initial-value problem is solved using Laplace transforms; causality is imposed. In the frequency domain (time-harmonic oscillations), a radiation condition is imposed: a plane-wave (Fourier) decomposition is used in which waves with outgoing group velocity are selected. It is shown that both appr… Show more

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Cited by 14 publications
(12 citation statements)
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“…This is our radiation condition. It has been used previously [3,24], and it has been shown to be consistent with causality in the time-domain [21]. As a result,…”
mentioning
confidence: 79%
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“…This is our radiation condition. It has been used previously [3,24], and it has been shown to be consistent with causality in the time-domain [21]. As a result,…”
mentioning
confidence: 79%
“…The total energy transported away, E out , is found by integrating over the beam cross-section [21,31]: The remaining integral is (4/a)K(k) sec θ c using (6.3), whence E out = E in (see (8.2)), as expected. We conclude by noting that results for a circular piston are readily obtained by setting a = b (k = 0).…”
Section: 7] Givesmentioning
confidence: 98%
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“…Earlier, efforts were made to remove the logarithmic singularity embedded in the integral representation (22) before applying the final boundary condition. As a result the integro-differential operator K emerged in (30) having a singular component and a regular part.…”
Section: Methodsmentioning
confidence: 99%
“…Furthermore, results show that the system of equations converges rapidly with increasing truncation size. This general approach forms the basis of recent work on similar problems involving submerged plates by [7] and has similarities to work by [8] for radiation of internal gravity waves by discs oscillating in a stratified fluid and [9] for scattering of surface waves by cracks in elastic solids.…”
Section: Introductionmentioning
confidence: 99%