On the Importance of Weak Steady Shear in the Refraction of Short Internal Waves

Ray theory is used to study the refraction of short oceanic internal waves by a spectrum of large amplitude inertia waves superimposed on a weakly sheared steady current. The results suggest that the steady current has a significant cumulative effect on short-wave propagation over the timescale of a...

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Hauptverfasser: Buckley, Greg, Broutman, Dave, Rottman, James W, Eckermann, Stephen
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creator Buckley, Greg
Broutman, Dave
Rottman, James W
Eckermann, Stephen
description Ray theory is used to study the refraction of short oceanic internal waves by a spectrum of large amplitude inertia waves superimposed on a weakly sheared steady current. The results suggest that the steady current has a significant cumulative effect on short-wave propagation over the timescale of a few inertia periods. The strength of ray convergence is also computed, as this affects short-wave amplitudes. Typically we find weak ray convergence and much slower growth toward instability with increasing vertical wavenumber than in a steady-shear critical-layer model. Published in Geophysical Research Letters, v26 n18 p2877-2880, 15 Sep 1999.
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source DTIC Technical Reports
subjects BUOYANCY
CONVERGENCE
GEOSTROPHIC CURRENTS
INERTIA
INTERNAL WAVES
OCEAN WAVES
Optics
Physical and Dynamic Oceanography
RAY CONVERGENCE
RAY THEORY
REFRACTION
REPRINTS
SECONDARY WAVES
STEADY CURRENTS
STEADY SHEAR
WAVE PROPAGATION
WAVENUMBERS
title On the Importance of Weak Steady Shear in the Refraction of Short Internal Waves
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