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- W2069851552 abstract "The numerical modeling of stratospheric, quasi-geostrophic Rossby wave propagation on a beta-plane channel is examined to determine how wave propagation is affected by the use of low horizontal (spectral) resolution. This study considers time dependent, quasi-linear, wave-mean flow interaction for typical wintertime conditions. Time dependent, wave-mean flow interaction modeling can show nonlinear behavior equivalent to quasi-horizontal planetary wavebreaking. Wave-mean flow interaction modeling requires relatively higher meridional resolution than is needed for the linear wave case because meridionally localized wave-mean flow interaction generally occurs. The interaction is viewed in terms of quasi-geostrophic potential vorticity on isobaric surfaces. The degree to which quasi-geostrophic potential vorticity is conserved locally as it is mixed quasi-horizontally by planetary waves under adiabatic conditions can be estimated by examining the evolution of the isobaric quasi-geostrophic potential vorticity, and this mixing is related to wave propagation by means of the Eliassen-Palm flux. It is shown that at lowest meridional resolution, where a single spectral mode is used to represent all meridional profiles, it is best to consider the channel model to be two dimensional in (x, z)." @default.
- W2069851552 created "2016-06-24" @default.
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- W2069851552 date "1988-01-01" @default.
- W2069851552 modified "2023-10-18" @default.
- W2069851552 title "Rossby Wave Propagation an Beta-Planes" @default.
- W2069851552 doi "https://doi.org/10.1175/1520-0469(1988)045<0041:rwpabp>2.0.co;2" @default.
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