Edge waves produced by the motion of a vessel in an ice channel
DOI10.1134/S0021894419050080zbMath1446.76084OpenAlexW2998090279WikidataQ126567289 ScholiaQ126567289MaRDI QIDQ2190172
Publication date: 18 June 2020
Published in: Journal of Applied Mechanics and Technical Physics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1134/s0021894419050080
Fourier transformWiener-Hopf techniquedispersion relationviscoelastic platewave forceflexural-gravity surface wave
Hydrology, hydrography, oceanography (86A05) Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Glaciology (86A40)
Cites Work
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- Action of a local time-periodic load on an ice sheet with a crack
- Motion of an external load over a semi-infinite ice sheet in the subcritical regime
- Behavior of a semi-infinite ice cover under a uniformly moving load
- Wave pattern due to a load moving on the free surface of a fluid along the edge of an ice sheet
- Wave motion in an ice sheet with crack under uniformly moving load
- The deformations and stresses in floating ice plates
- Wave scattering by narrow cracks in ice sheets floating on water of finite depth
- Trapping of waves by thin floating ice floes
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