On Damped Resonant InteractionsSource: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 010::page 1677Author:Miles, John
DOI: 10.1175/1520-0485(1984)014<1677:ODRI>2.0.CO;2Publisher: American Meteorological Society
Abstract: It 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.
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| contributor author | Miles, John | |
| date accessioned | 2017-06-09T14:47:15Z | |
| date available | 2017-06-09T14:47:15Z | |
| date copyright | 1984/10/01 | |
| date issued | 1984 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-26767.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4163697 | |
| description abstract | It 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. | |
| publisher | American Meteorological Society | |
| title | On Damped Resonant Interactions | |
| type | Journal Paper | |
| journal volume | 14 | |
| journal issue | 10 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1984)014<1677:ODRI>2.0.CO;2 | |
| journal fristpage | 1677 | |
| journal lastpage | 1678 | |
| tree | Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 010 | |
| contenttype | Fulltext |