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Hydroelastic waves induced by initial disturbances in ice-covered waters with currents
Indra Mani Prasad1, Harekrushna Behera2
1Department of Mathematics, SRM Institute of Science and Technology, 603203, Kattankulathur, Tamil Nadu, India.
Flexural-gravity waves generated in ice-covered fluids are influenced by uniform currents and ice rigidity. Increased current speed amplifies wave depression, while greater ice rigidity reduces it.
Area of Science:
- Fluid dynamics
- Geophysics
- Solid mechanics
Background:
- Ice-covered fluids generate complex wave phenomena.
- Uniform currents significantly alter wave propagation characteristics.
- Flexural rigidity of ice impacts surface wave dynamics.
Purpose of the Study:
- Investigate flexural-gravity wave generation in an infinite-depth fluid.
- Analyze the influence of uniform currents and ice cover properties.
- Examine two distinct initial disturbance types: initial displacement and impulsive load.
Main Methods:
- Utilized Laplace and Fourier transformations for precise integral representation.
- Applied the stationary phase technique for asymptotic evaluation over large time and distance.
- Examined effects of flexural rigidity and current speed on wave depression.
Main Results:
- Depression height increases with rising current speed.
- Increased ice cover rigidity substantially decreases displacement amplitude.
- Impulsive loading results in significantly larger depression amplitude than initial displacement.
Conclusions:
- Wave generation in ice-covered fluids is sensitive to current and ice properties.
- The nature of initial disturbance critically affects wave amplitude.
- Findings provide insights into geophysical fluid dynamics and ice mechanics.
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