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Asymmetric internal solitary waves with a trapped core in deep fluids
preprint
posted on 2007-02-28, 12:01 authored by Oleg G. Derzho, Roger GrimshawWe describe an asymptotic model for long large-amplitude internal solitary waves
with a trapped core, propagating in a narrow layer of nearly uniformly stratified fluid
embedded in an infinitely deep homogeneous fluid. We consider the case of a mode
one asymmetric wave with an amplitude slightly greater than the critical amplitude,
for which there is incipient over-turning, that is wave-breaking. We then incorporate
a vortex core located near the point at which this incipient breaking occurs. The effect
of the vortex core is to introduce into the governing equation for the wave amplitude
an extra nonlinear term proportional to the 3/2 power of the difference between the
wave amplitude and the critical amplitude. Thus the derived new equation for the
wave amplitude incorporates both the nonlinearity arising due to the flow over the
recirculation core, and the nonlinearity associated with the ambient stratification;
the dispersion term however remains of the Benjamin-Ono type. We find that as the
wave amplitude increases above the critical amplitude, the wave broadens, which is
in marked contrast to the case of small amplitude waves where a sharpening of the
wave crest normally occurs. The limiting form of the broadening wave is “a deep
fluid bore”. The wave speed is found to depend nonlinearly on the wave amplitude
and the traditional linear dependence underestimates this speed.
History
School
- Science
Department
- Mathematical Sciences
Pages
305361 bytesPublication date
2007Notes
This is a pre-print.Language
- en