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contributor authorMiles, John
date accessioned2017-06-09T14:47:15Z
date available2017-06-09T14:47:15Z
date copyright1984/10/01
date issued1984
identifier issn0022-3670
identifier otherams-26767.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163697
description abstractIt is shown that the evolution equations for a triad of weakly damped, resonantly interacting waves are isomorphic to the corresponding equations for undamped waves (and therefore may be integrated in term of elliptic functions) if the damping coefficient is the same for each member of the triad. This condition is satisfied for topographic Rossby waves for which dissipation is through a turbulent Ekman layer and the wavelengths are small compared with the Rossby radius of deformation.
publisherAmerican Meteorological Society
titleOn Damped Resonant Interactions
typeJournal Paper
journal volume14
journal issue10
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1984)014<1677:ODRI>2.0.CO;2
journal fristpage1677
journal lastpage1678
treeJournal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 010
contenttypeFulltext


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