Modeling of nonmigrating tides in the middle atmosphere
On the basis of calculations using the general circulation model of the middle and upper atmosphere, the relative role of sources of nonmigrating tides distributed in atmosphere has been investigated. It is shown that in winter, when planetary waves in stratosphere are well developed, the main contr...
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| Veröffentlicht in: | Geomagnetism and Aeronomy 2011-02, Vol.51 (1), p.105-115 |
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| creator | Suvorova, E. V. Pogoreltsev, A. I. |
| description | On the basis of calculations using the general circulation model of the middle and upper atmosphere, the relative role of sources of nonmigrating tides distributed in atmosphere has been investigated. It is shown that in winter, when planetary waves in stratosphere are well developed, the main contribution to the generation of nonmigrating tides is caused by nonlinear interaction between migrating tides and a quasi-stationary planetary wave with zonal wave number 1 (SPW1). Taking into account the longitudinal ozone inhomogeneities in the model leads to the occurrence of additional sources of nonmigrating tides caused by longitudinally inhomogeneous heating of the atmosphere, the contribution of which can be comparable to that from nonlinear interaction under an attenuating amplitude of SPW1 in the stratosphere. |
| doi_str_mv | 10.1134/S0016793210061039 |
| format | Article |
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| source | SpringerLink Journals - AutoHoldings |
| subjects | Aeronomy Atmosphere Earth and Environmental Science Earth Sciences General circulation models Geophysics Geophysics/Geodesy Stratosphere Tides Upper atmosphere |
| title | Modeling of nonmigrating tides in the middle atmosphere |
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