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• W2056959050 abstract "Abstract The present note proposes an explanation of topographic normal modes that grow in a flow with a zonally symmetric mountain. An issue of practical importance is whether one expects the maximum amplitude to occur poleward or equatorward of a mountain localized in the cross-stream direction. Using a quasigeostrophic model, it is shown that the occurrence of maximum amplitude to the south of the mountain occurs only for longer waves. For a given wave of medium scale, the amplitude is more likely to maximize to the south of the mountain for steeper slopes. The transient behavior resulting from the sudden appearance of a mountain in the presence of an Eady normal mode is discussed first. The topographic correction to the Eady mode quickly acquires a negative meridional tilt at the surface. This tilted structure penetrates upward to the lid and advects basic-state temperature. Because the phase tilt of the Eady mode varies with zonal wavelength, the phase of the topographic correction at the lid relativ..." @default.
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• W2056959050 date "1999-09-01" @default.
• W2056959050 modified "2023-09-28" @default.
• W2056959050 title "The Transition to Topographic Normal Modes" @default.
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• W2056959050 doi "https://doi.org/10.1175/1520-0469(1999)056<3321:ttttnm>2.0.co;2" @default.
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