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contributor authorBrown, Ellen D.
contributor authorOwens, W. Brechner
date accessioned2017-06-09T14:46:01Z
date available2017-06-09T14:46:01Z
date copyright1981/11/01
date issued1981
identifier issn0022-3670
identifier otherams-26298.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163176
description abstractMomentum and energy transfers from the mesoscale horizontal velocity shear to the internal wave field have been deduced from an analysis of a closely spaced, 25 km, moored current-meter array. The correlation between the low-frequency horizontal shear and internal-wave-field continuum effective stress implies a significant horizontal eddy viscosity of O (106 cm2 s?1), somewhat larger than predicted by Müller (1976). A simple steady-state energy balance for the internal wave field using the observed correlation between the internal wave kinetic energy and the square of the low-frequency shear implies a 10-day relaxation time for the internal-wave Acid and a combined vertical viscosity and horizontal diffusivity not significantly different from zero. These estimates are within the experimental uncertainty of previous observational analyses.
publisherAmerican Meteorological Society
titleObservations of the Horizontal Interactions between the Internal Wave Field and the Mesoscale Flow
typeJournal Paper
journal volume11
journal issue11
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1981)011<1474:OOTHIB>2.0.CO;2
journal fristpage1474
journal lastpage1480
treeJournal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 011
contenttypeFulltext


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