Comments on the Gravity Wave Theory of J. Weinstock Concerning Dissipation Induced by Nonlinear Effects
It has been alleged that gravity waves having large vertical wavenumbers in the middle atmosphere are subject to dissipation by a diffusivity engendered by other waves via nonlinear wave-wave interaction, with the diffusivity taking a very particular, specified form. Here it is argued that the putat...
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| Published in | Journal of the atmospheric sciences Vol. 59; no. 12; pp. 2024 - 2030 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Boston, MA
American Meteorological Society
15.06.2002
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0022-4928 1520-0469 |
| DOI | 10.1175/1520-0469(2002)059<2024:COTGWT>2.0.CO;2 |
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| Abstract | It has been alleged that gravity waves having large vertical wavenumbers in the middle atmosphere are subject to dissipation by a diffusivity engendered by other waves via nonlinear wave-wave interaction, with the diffusivity taking a very particular, specified form. Here it is argued that the putative diffusivity was inferred on improper physical assumptions and mathematical developments. |
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| AbstractList | It has been alleged that gravity waves having large vertical wavenumbers in the middle atmosphere are subject to dissipation by a diffusivity engendered by other waves via nonlinear wave-wave interaction, with the diffusivity taking a very particular, specified form. Here it is argued that the putative diffusivity was inferred on improper physical assumptions and mathematical developments. The conclusion has implications for the modeling of the general circulation of the middle atmosphere. (Author) It has been alleged that gravity waves having large vertical wavenumbers in the middle atmosphere are subject to dissipation by a diffusivity engendered by other waves via nonlinear wave-wave interaction, with the diffusivity taking a very particular, specified form. Here it is argued that the putative diffusivity was inferred on improper physical assumptions and mathematical developments. |
| Author | Hines, Colin O. |
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| DOI | 10.1175/1520-0469(2002)059<2024:COTGWT>2.0.CO;2 |
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| Keywords | Theoretical study Stratosphere Wave interaction Non linear effect Gravity wave |
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| SubjectTerms | Atmosphere Climate change Earth, ocean, space Exact sciences and technology External geophysics Gravity Gravity waves Meteorology Physics of the high neutral atmosphere Tides, waves, convection, winds, turbulence |
| Title | Comments on the Gravity Wave Theory of J. Weinstock Concerning Dissipation Induced by Nonlinear Effects |
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