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Permanent link (DOI): https://doi.org/10.7939/R3XS5JP90

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Anelastic Internal Wave Reflection and Transmission in Uniform Retrograde Shear Open Access

Descriptions

Other title
Subject/Keyword
Stratified Flow
Wave Reflection
Internal Waves
Type of item
Thesis
Degree grantor
University of Alberta
Author or creator
Eberly, Lauren E
Supervisor and department
Bruce R. Sutherland Physics/Earth and Atmosphere Science
Examining committee member and department
Gordon E. Swaters Applied Mathematics
Andrew B.G. Bush Earth and Atmosphere Science
Department
Department of Earth and Atmospheric Sciences
Specialization

Date accepted
2014-05-02T14:26:47Z
Graduation date
2014-11
Degree
Master of Science
Degree level
Master's
Abstract
We perform fully nonlinear simulations in two dimensions of a horizontally periodic, vertically localized, anelastic internal wavepacket in order to examine the effects of weak and strong nonlinearity upon wavepackets approaching a reflection level in uniform retrograde shear. Transmission, reflection and momentum deposition are measured in terms of the horizontal momentum associated with the wave-induced mean flow. These are determined in part as they depend upon the initial wavenumber vector, ⃗k = (k,m), which determines the modulational stability (if |m/k| > 0.7) or instability (if |m/k| < 0.7) of moderately large amplitude quasi-monochromatic internal wavepackets. Whether modulationally stable or unstable, the evolution of the wavepacket is determined by the height of the reflection level predicted by linear theory, zr, relative to the height, z∆, at which weak nonlinearity becomes significant, and the height, zb > z∆, at which linear theory predicts anelastic waves first overturn in the absence of shear. If zr < z∆, the amplitude remains sufficiently small and the waves reflect as pre- dicted by linear theory. If zr is moderately larger than z∆, a fraction of the momentum associated with the wavepackets transmits past the reflection level. This is because the positive shear associated with the wave-induced mean flow can partially shield the wavepacket from the influence of the negative background shear enhancing its transmission. The effect is enhanced for weakly nonlinear modulationally unstable wavepackets that narrow and grow in amplitude faster than the anelastic growth rate. However, as nonlinear effects become more pro- nounced, a significant fraction of the momentum associated with the wavepacket is irreversibly deposited to the background below the reflection level. This is particularly the case for modulationally unstable wavepackets, whose enhanced amplitude growth leads to overturning below the predicted breaking level. Be- cause the growth in the amplitude envelope of modulationally stable wavepackets is retarded by weakly nonlinear effects, reflection is enhanced and transmission retarded relative to their modulationally unstable counterparts. Applications to mountain wave propagation through the stratosphere in the winter hemisphere are discussed as well as applications of a fully nonlinear, anelastic wave model to non-constant buoyancy frequency backgrounds.
Language
English
DOI
doi:10.7939/R3XS5JP90
Rights
Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission.
Citation for previous publication
L.Eberly, B.R. Sutherland “Anelastic internal wave reflection and transmission in uniform retrograde shear,” Physics of Fluids, vol. 26, 026601.

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