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    Rossby Waves in Zonal Barotropic Flows with Pseudocritical Levels 

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 018:;page 2665
    Author(s): Harlander, Uwe
    Publisher: American Meteorological Society
    Abstract: A pseudocritical level is defined as a region where the wave phase speed c equals the zonal basic flow velocity U and, additionally, the background potential vorticity gradient vanishes. In this study Rossby wave propagation ...
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    Transition from Geostrophic Flows to Inertia–Gravity Waves in the Spectrum of a Differentially Heated Rotating Annulus Experiment 

    Source: Journal of the Atmospheric Sciences:;2020:;volume( 77 ):;issue: 008:;page 2793
    Author(s): Rodda, Costanza;Harlander, Uwe
    Publisher: American Meteorological Society
    Abstract: Inertia–gravity waves (IGWs) play an essential role in the terrestrial atmospheric dynamics as they can lead to energy and momentum flux when propagating upward. An open question is to what extent IGWs contribute to the ...
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    On Quasigeostrophic Normal Modes in Ocean Models: Weakly Nonseparable Situation 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 009:;page 2086
    Author(s): Harlander, Uwe; Maas, Leo R. M.
    Publisher: American Meteorological Society
    Abstract: This study examines quasigeostrophic Rossby eigenmodes of homogeneous as well as stratified oceans. Analytical studies of Rossby basin modes are usually done by using simple basin geometries. Simple means that solutions ...
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