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    The Interaction of Two Internal Waves with the Mean Flow: Implications for the Theory of the Quasi-Biennial Oscillation 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 012:;page 1847
    Author(s): Plumb, R. A.
    Publisher: American Meteorological Society
    Abstract: Internal waves propagating through a dissipative fluid interact with the mean flow. In response to forcing by a single wave, the mean flow evolves to a steady solution. In the presence of two (or more) waves such a solution ...
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    Eddy Fluxes of Conserved Quantities by Small-Amplitude Waves 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 009:;page 1699
    Author(s): Plumb, R. A.
    Publisher: American Meteorological Society
    Abstract: General kinematical arguments are used to derive certain properties of eddy fluxes of conserved quantities in a field of small-amplitude waves. The direction of the eddy flux is related in a simple way to wave transience ...
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    Forced Waves in a Baroclinic Shear Flow. Part I: Undamped Evolution near the Baroclinic Instability Threshold 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 002:;page 205
    Author(s): Plumb, R. A.
    Publisher: American Meteorological Society
    Abstract: The properties of forced waves in a two-layer baroclinic fluid are considered. The mean shear is taken to be just smaller than the critical value required for baroclinic instability. A nonlinear evolution equation is derived ...
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    The Zonally Averaged Transport Characteristics of the GFDL General Circulation/Transport Model 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 002:;page 298
    Author(s): Plumb, R. A.; Mahlman, J. D.
    Publisher: American Meteorological Society
    Abstract: The GFDL general circulation/tracer model has been used to generate the transport coefficients required in two-dimensional (zonally averaged) transport formulations. This was done by assuming a flux-gradient relationship ...
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    The Instability of a Forced Standing Wave in a Viscous Stratified Fluid: A Laboratory Analogue of .the Quasi-Biennial Oscillation 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 010:;page 1827
    Author(s): Plumb, R. A.; McEwan, A. D.
    Publisher: American Meteorological Society
    Abstract: An experiment is described in which a standing internal wave is forced at the lower boundary of an annulus of salt-stratified water. At sufficiently large forcing amplitudes, the wave motion generates a strong mean azimuthal ...
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    Nonlinear, Barotropic Response to a Localized Topographic Forcing: Formation of a “Tropical Surf Zone” and Its Effect on Interhemispheric Propagation 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 011:;page 1401
    Author(s): Waugh, D. W.; Plumb, R. A.; Polvani, L. M.
    Publisher: American Meteorological Society
    Abstract: The nonlinear response of a barotropic, nondivergent, spherical flow representative of the upper troposphere (but without a tropical Hadley cell) to localized, extratropical topographic forcing is examined using high-resolution ...
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    The Quasi-Two-Day Wave Event of January 1984 and Its Impact on the Mean Mesospheric Circulation 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020:;page 3030
    Author(s): Plumb, R. A.; Vincent, R. A.; Craig, R. L.
    Publisher: American Meteorological Society
    Abstract: Studies of the quasi-two-day wave show that it is a summertime phenomenon. In the summer of 1983?84 at Adelaide (35°S, 138°E), the main phase of the wave appeared as a pulse in mid-January which lasted about seven cycles ...
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    Methods of Calculating Transport across the Polar Vortex Edge 

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 018:;page 2241
    Author(s): Sobel, A. H.; Plumb, R. A.; Waugh, D. W.
    Publisher: American Meteorological Society
    Abstract: Existing quantitative calculations of material transport across the stratospheric polar vortex edge are difficult to interpret. This is because what is actually calculated has not been clearly shown to be irreversible ...
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    Thermal Convection in a Rotating Fluid Subject to a Horizontal Temperature Gradient: Spatial and Temporal Characteristics of Fully Developed Baroclinic Waves 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 006:;page 930
    Author(s): Hide, R.; Mason, P. J.; Plumb, R. A.
    Publisher: American Meteorological Society
    Abstract: Detailed studies of the azimuthal structure of fully developed waves in a differentially heated rotating fluid annulus have been carried out with the aid of instrumentation capable of providing frequent determinations of ...
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