Abstract:
Scattering and resonance in water waves are fundamentally important for both scienti c
understanding and practical applications in oceanography, coastal engineering, and
environmental
uid mechanics. This thesis investigates the scattering and resonance
behavior of surface and internal water waves interacting with non-uniform bathymetries.
Studying wave scattering over non-uniform bathymetries is not only scienti cally rich but
also practically indispensable. Few problems involves the presence of
oating structures
both in the absence and presence of bathymtery. This allows for employing a range
of mathematical techniques in order to solve the boundary value problems arising in
various problems considered here. The analysis of
oating structures in conjunction
with non-uniform bathymetries provide a comprehensive framework to understand and
design advanced coastal protection systems, e cient wave energy harvesting setups,
realistic models for wave-induced transport and predictive tools for o shore structural
stability. Focusing on non-uniform bottom con gurations, as well as single, two, and
three-layer
uid systems, the study presents a uni ed approach to understanding wave
dynamics in realistic oceanographic environments. These wave interactions are crucial
for understanding wave energy dissipation, re
ection, and transmission patterns, which
directly impact coastal erosion, sediment transport, and the stability of maritime
structures. Under the umbrella of linearised water wave theory along with certain
assumptions, the problems in each chapter results into a mixed boundary value problem.
The complexity in these boundary value problems requires sophisticated mathematical
and computational techniques, and this study employs several advanced methods like
Multi-scale analysis, Boundary element method, Eigenfunction expansion method and
Integral equation method to analyze and solve these mixed boundary value problems
arising from the water wave scattering problems.
The thesis begins with the analytical modeling of Bragg resonance phenomena using
multi-scale perturbation analysis for non-uniform seabeds. In another work, we consider
the Class II Bragg resonance which requires the bottom to be the combination of two
sinusoids resembling a uneven bathymetry.
The study then transitions to scattering by array of non-uniform rigid barriers over
at seabed, utilizing Eigenfunction expansion method and Boundary element method.
Various arrangements of the barriers with unequal draft are investigated to optimize wave
re
ection, revealing that monotonically varying bar con gurations signi cantly enhance
wave attenuation through Bragg scattering. We also examine another study when a rigid
barrier is present over non-uniform oscillatory seabed in order to see their combined e ect
of wave re
ection and transmission.
A further extension to step-type bathymetries which represents the continental shelves
is taken. Integral equation approach followed by Galerkin techniques are employed which incorporate the e ect of cube root singularity at the edge of the corner and then further
approximated by general polynomial whose weight function can be chosen suitably
depending upon the above singularity present in the system. Same technique is employed
to the problem involving a rigid thin barrier over a step type of bottom where both cube
root singularity at the edge of the step and square root singularity at the edge of barrier
are taken into account. Re
ection and transmission coe cients are obtained for obliquely
incident waves.
The thesis also addresses internal wave dynamics and Bragg resonance in strati ed
two-layer systems, analyzing weakly nonlinear e ects and interfacial mode behavior over
non-uniform oscillatory bottoms using the method of perturbation and followed by Fourier
transform technique. Lastly, in a shift from scattering to transport phenomena,
uid
particle trajectories in a three-layer system are studied under the in
uence of interfacial
tension and density strati cation. The analysis reveals non-monotonic trajectory behavior
across layers, in
uenced by varying density ratios and interface interactions. The closed
trajectories are analysed using small-excursion principle.
In all problems, results are validated by comparing with available results as far as
possible which proves the e ectiveness of the present models. Also, in all the problem,
the numerical results are plotted through graphs to analyze the e ect of di erent system
and wave parameters.