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    A Linear Model of the Walker Circulation 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 007:;page 1390
    Author(s): Geisler, J. E.
    Publisher: American Meteorological Society
    Abstract: In this paper we present results of a model study of the Walker Circulation defined as the steady response of a stratified atmosphere to an isolated equatorial heat source. The model equations are linearized with respect ...
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    On the Vertical Distribution of Latent Heat Release and the Mechanics of CISK 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 002:;page 240
    Author(s): Geisler, J. E.
    Publisher: American Meteorological Society
    Abstract: A simple two-dimensional model is used to demonstrate the importance of the vertical distribution of latent heat release for the functioning of CISK, When the horizontal scale of the prescribed heat source in the model is ...
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    The Effect of East African Topography on Flow Driven by Zonally Symmetric Forcing 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 017:;page 1862
    Author(s): Paegle, Jan; Geisler, J. E.
    Publisher: American Meteorological Society
    Abstract: The low-level circulation in summer over the western Indian Ocean is characterized by southeast trades that are channeled near the African coast into a concentrated southerly flow across the equator and thence north-eastward ...
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    The Role of Variable Coriolis Parameter in the Propagation of Inertia-Gravity Waves During the Process of Geostrophic Adjustment 

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 003:;page 263
    Author(s): Geisler, J. E.; Dickinson, R. E.
    Publisher: American Meteorological Society
    Abstract: This analysis treats the transient inertia-gravity wave response of a shallow fluid to an impulsive addition of momentum. The Coriolis parameter varies with latitude, but Rossby waves are not considered. The square of the ...
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    Comment on “Upper-Atmosphere Sodium and Stratospheric Warmings at High Latitudes” 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 006:;page 720
    Author(s): Geisler, J. E.; Dickinson, R. E.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    VERTICAL MOTION FIELD IN THE MIDDLE THERMOSPHERE FROM SATELLITE DRAG DENSITIES 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 009:;page 606
    Author(s): DICKINSON, R. E.; GEISLER, J. E.
    Publisher: American Meteorological Society
    Abstract: The vertical motion field in the thermosphere is calculated from the continuity equation. This calculation is based on a field of horizontal winds and an intermediate model of the thermospheric temperature field consistent ...
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    The Sea-Breeze Forerunner 

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 001:;page 82
    Author(s): Geisler, J. E.; Bretherton, F. P.
    Publisher: American Meteorological Society
    Abstract: The response of a stably stratified atmosphere to differential heating across a coastline is studied. A linear, inviscid, Boussinesq theory is used to analyze the growth caused by switching on a small temperature contrast ...
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    Numerical Study of an Interacting Rossby Wave and Barotropic Zonal Flow Near a Critical Level 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 004:;page 946
    Author(s): Geisler, J. E.; Dickinson, R. E.
    Publisher: American Meteorological Society
    Abstract: This paper treats the initial value problem of a forced Rossby wave encountering a critical level in a barotropic zonal shear flow which can change in response to the wave momentum flux divergence. The main result of the ...
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    The Five-Day Wave on a Sphere with Realistic Zonal Winds 

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 004:;page 632
    Author(s): Geisler, J. E.; Dickinson, Robert E.
    Publisher: American Meteorological Society
    Abstract: A 5-day zonal wavenumber 1 oscillation has been well-documented from analysis of surface pressure data, and it has been suggested that it corresponds to the gravest symmetric low-frequency external normal mode of the ...
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