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Waves generated by two or more ships in a channel
(2010-12-01)
The numerical model FUNWAVE+Ship simulates the generation and propagation of ship waves to shore, including phenomena such as refraction, diffraction, currents and breaking of waves. The interaction of two wave trains, ...
Waves generated by two or more ships in a channel
(2010-12-01)
The numerical model FUNWAVE+Ship simulates the generation and propagation of ship waves to shore, including phenomena such as refraction, diffraction, currents and breaking of waves. The interaction of two wave trains, ...
Propagation of ship waves on a sloping bottom
(2009-12-01)
The numerical model FUNWAVE was adapted in order to simulate the generation and propagation of ship waves to shore, including phenomena such as refraction, diffraction, currents and breaking of waves. Results are shown for ...
Propagation of ship waves on a sloping bottom
(2009-12-01)
The numerical model FUNWAVE was adapted in order to simulate the generation and propagation of ship waves to shore, including phenomena such as refraction, diffraction, currents and breaking of waves. Results are shown for ...
Atlantik-wellen (Atlantic Waves)
(2009-04-29)
The title of this postcard is German for "Atlantic Waves" which describes the large swells in the photograph.
Asymptotic approach for the nonlinear equatorial long wave interactions
(2011-08-30)
In the present work we use an asymptotic approach to obtain the long wave equations. The shallow water equation is put as a function of an external parameter that is a measure of both the spatial scales anisotropy and the ...
Asymptotic approach for the nonlinear equatorial long wave interactions
(2011-08-30)
In the present work we use an asymptotic approach to obtain the long wave equations. The shallow water equation is put as a function of an external parameter that is a measure of both the spatial scales anisotropy and the ...
Analytical partial derivatives of the phase- and group Velocities for rayleigh waves propagating in a layer on a half-space
(2005)
The dispersion relation for Rayleigh waves in a layer on a half-space is modified by
introducing the quadratic wave number instead of the phase velocity. The implicit
function theorem is then used to derive analytical ...
Spherical seismic waves
(2016)