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    Baroclinic Instability at Short Wavelengths in Vertically Discrete Quasi-Geostrophic and Ageostrophic Models 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 021:;page 3305
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: Short wavelength linear baroclinic instability is examined numerically in two quasi-geostrophic models and one ageostrophic model. The growth rate spectra for the ageostrophic model differ little from those of the ...
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    Baroclinic Instability and Isentropic Slope 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 009:;page 1133
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: The wavelength of maximum baroclinic instability (WMI), maximum growth rate (MGR), phase velocities, and other quantities, are computed for an atmosphere with an internal 100-mb layer having various shears and lapse rates ...
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    Baroclinic Instability in the Upper Troposphere 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 021:;page 3298
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: Observations show that the lapse rate increases upward in the troposphere. Baroclinic instability spectra are presented for the lapse rate increasing linearly upward from small values in the lower troposphere to large ...
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    Ageostrophic Subsynoptic-Scale Baroclinic Instability 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 019:;page 3065
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: The discrete-level baroclinic eigenproblem developed by Satyamurty et al., based on a Boussinesq primitive equation model, is solved by a shooting method for very high vertical resolution. It is found that the vertical ...
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    Boundary-Layer Damping of Baroclinic Instability 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 005:;page 772
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: A shooting method is applied to a 100-level perturbation model with an explicit Ekman layer. Growth rates for a no-slip boundary condition are similar to those found previously. It is noted that the large cross-isobaric ...
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    A Partial Theory of the 26-Month Oscillation of the Zonal Wind in the Equatorial Stratosphere 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 006:;page 506
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: Attempted explanations of the 26-month zonal wind oscillation in the equatorial stratosphere are critically examined. Explanations in terms of subharmonic response, ?vacillation,? or a resonant mode are rejected. Some ...
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    Stratospheric Mass Variations and Fission Product Radioactivity in Surface Air 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 006:;page 615
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    AN EVALUATION OF CERTAIN FORMS OF MOMENTUM TRANSFER IN THE 26-MONTH OSCILLATION 

    Source: Monthly Weather Review:;1965:;volume( 093 ):;issue: 003:;page 157
    Author(s): STALEY, D. O.
    Publisher: American Meteorological Society
    Abstract: The fundamental equations are linearized by the method of small perturbations for the conditions of hydrostatic equilibrium and geostrophic balance of meridional forces. In a first case, Fickian momentum diffusion is used; ...
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    The Adiabatic Lapse Rate in the Venus Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 002:;page 219
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: The adiabatic lapse rate is derived for a real gas, and the result applied to the Venus atmosphere, which is assumed to consist of pure CO2. The ratio of the real to the ideal gas adiabatic lapse rate is found to exceed ...
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    Climatology of Sr-90 in Surface Air: A Simple Model using Diffusion and Scavenging 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 001:;page 36
    Author(s): Staley, D. O.
    Publisher: American Meteorological Society
    Abstract: The evolution of Sr-90 distribution following an instantaneous stratospheric or tropospheric source in an annulus defined by latitude walls is investigated by means of a very simple model that uses 12 stratospheric and 12 ...
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