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contributor authorMunk, W.
contributor authorWorcester, P.
contributor authorZachariasen, F.
date accessioned2017-06-09T14:45:49Z
date available2017-06-09T14:45:49Z
date copyright1981/04/01
date issued1981
identifier issn0022-3670
identifier otherams-26208.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163077
description abstractInternal waves scatter sound by two related perturbations: 1) those associated with vertical particle displacements ?(x, y, z, t) in the presence of a vertical gradient of (potential) sound speed (δc = ??zcp); and 2) those associated with horizontal particle velocities u(x, y, z, t). The combined fractional perturbation in propagation velocity is δc/c + u/c. The second term, generally neglected, introduces a nonreciprocity when source and receiver are interchanged. Nonreciprocity is expected to be relatively small except for transmission along a deep downward loop. The principal internal wave contribution to nonreciprocity is from inertial frequencies. The sum and difference of reciprocal travel times are a measure of ? and u, respectively, along the ray path,, the quadrature spectrum of reciprocal travel times is related by an integral equation to the spectrum of the momentum flux ??u?. Precise measurements of nonreciprocity could provide an estimate of the vertical momentum flux in an internal wave field.
publisherAmerican Meteorological Society
titleScattering of Sound by Internal Wave Currents: The Relation to Vertical Momentum Flux
typeJournal Paper
journal volume11
journal issue4
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1981)011<0442:SOSBIW>2.0.CO;2
journal fristpage442
journal lastpage454
treeJournal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 004
contenttypeFulltext


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