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Flexural gravity wave generation by initial disturbances in the presence of current

TLDR
In this paper, the effect of uniform current on the generation of flexural gravity waves resulting from initial disturbances at a point was analyzed in two dimensions, where the problem was formulated as an initial boundary value problem under the assumptions of the linearized theory of water waves by direct application of the Laplace transform and then the Fourier transform.
Abstract
The effect of uniform current on the generation of flexural gravity waves resulting from initial disturbances at a point was analyzed in two dimensions The problem was formulated as an initial boundary value problem under the assumptions of the linearized theory of water waves By direct application of the Laplace transform and then the Fourier transform, explicit expressions for the velocity potential and free surface elevation were obtained in integral forms; these were evaluated asymptotically for large distances and times by the application of the method of the stationary phase to obtain the far field behavior of the surface elevations in specific cases Simple numerical computations were performed to illustrate the effect of uniform current on the surface elevation, wavelength, phase velocity, and group velocity of the flexural gravity waves and on the far field behavior of the progressive waves in two different cases, namely, when there is an initial depression concentrated at the origin and an initial impulse concentrated at the origin

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Analytical Study of the Head-On Collision Process between Hydroelastic Solitary Waves in the Presence of a Uniform Current

TL;DR: An analytical simulation of the head-on collision between a pair of hydroelastic solitary waves propagating in the opposite directions in the absence of a uniform current finds that the presence of a current strongly affects the wavelength and wave speed of both solitary waves.
Journal ArticleDOI

Time dependent flexural gravity waves in the presence of current

TL;DR: In this article, a combined effect of current and compressive force on time dependent flexural gravity wave motion in both the cases of single and two-layer fluids is analyzed in finite and infinite water depths in two dimensions.
Journal ArticleDOI

Time-dependent wave motion with undulated bottom

TL;DR: In this paper, the authors analyzed the time-dependent capillary gravity wave motion in the presence of a current and an undulated permeable bottom, and the spectral method was used to simulate the timedependent surface elevation.
Journal ArticleDOI

Transient flexural gravity waves in two-layer fluid

TL;DR: In this paper, the effect of opposing current and critical compressive force in the presence of current has significant impact on the plate deflection, and integral forms of velocity potentials, structural deflection and interface elevations are derived.
Journal ArticleDOI

Time dependent wave motion in a permeable bed

TL;DR: In this article, the effect of current, compressive force and porosity parameter on phase and group velocities and floating plate deflection is analyzed using Laplace-Fourier transform method.
References
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Journal ArticleDOI

Waves due to a steadily moving source on a floating ice plate

TL;DR: In this article, steady wave patterns generated by a steadily moving source on a water-ice system that is assumed to be homogeneous and of infinite horizontal extent, using asymptotic Fourier analysis to give a simple description of the wave pattern far from the source.
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Waves due to a steadily moving source on a floating ice plate. Part 2

TL;DR: In this article, a two-layer model is used to describe stratification, which introduces a new system of slow internal waves associated with the layer interface, while the surface flexural waves are only slightly modified.
Journal ArticleDOI

The response of a floating ice sheet to an accelerating line load

TL;DR: In this article, the response of a thin, floating sheet of ice to a line load that accelerates from rest at t = 0 to a uniform velocity V for t ≥ T is determined through an integral-transform solution of the linearized equations of motion.
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