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    An Observational and Theoretical Study of Colorado Lee Cyclogenesis 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 013:;page 1541
    Author(s): Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: A cyclogenesis event that occurred over Colorado in early March of 1981 is the focus of this study. Two features that seemed to play a role in storm initiation were a traveling upper troposphere disturbance associated with ...
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    Radiatively Driven Interactions between Stratocumulus and Synoptic Waves 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 016:;page 2731
    Author(s): Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: Quasigeostrophic disturbances on a midlatitude ?-plane channel forced by radiative heating perturbations due to synoptic-scale variations of low-level stratiform cloud are considered. The longitudinal phase of the cloud ...
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    A QUASI-GEOSTROPHIC MODEL OF THE WINTER STRATOSPHERIC CIRCULATION 

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 006:;page 443
    Author(s): CLARK, JOHN H. E.
    Publisher: American Meteorological Society
    Abstract: A six-level quasi-geostrophic model including radiative and photochemical processes in the manner suggested by Lindzen and Goody is run from a state of joint radiative-photochemical equilibrium for midwinter conditions. ...
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    The Role of Kelvin Waves in Evolution of the Catalina Eddy 

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 005:;page 838
    Author(s): Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: The response to pressure falls near a coastline is studied with a linear shallow-water representation of the inversion-capped marine layer. The aim is to examine Catalina eddy development in the southern California bight ...
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    The Theory of the Vertical Propagation of Quasi-Geostrophic Disturbances in the Presence of Distorted Background Flows 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 012:;page 2217
    Author(s): Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: The structure and vertical propagation of a quasi-geostrophic disturbance in the presence of a constant zonal flow which has been distorted by a finite-amplitude forced stationary wave is considered. The vertical structure ...
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    The Vertical Propagation of Forced Atmospheric Planetary Waves 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 008:;page 1430
    Author(s): Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: Adiabatic, inviscid, quasi-geostrophic perturbations on a ? plane are forced at some initial time by the switch-on of a vertical velocity or temperature disturbance at the base of a stratified atmosphere. The vertical ...
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    Gravity Waves Driven by Diurnal Fluctuations in Mesoscale Heating 

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 005:;page 769
    Author(s): Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: Observed convective systems, such as mesoscale convective complexes (MCCs), often undergo repeated cycles of nocturnal growth and daytime decay especially during the summer. The gravity wave response to these pulsations ...
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    Resonant Planetary Waves in a Spherical Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 001:;page 20
    Author(s): Schoeberl, Mark R.; Clark, John H. E.
    Publisher: American Meteorological Society
    Abstract: A global model of planetary wave propagation in a spherical atmosphere is used to examine the spectrum of free or resonant planetary waves of the solstitial stratosphere. These free modes are located by forcing the model ...
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    The Catalina Eddy Event of July 1987: A Coastally Trapped Mesoscale Response to Synoptic Forcing 

    Source: Monthly Weather Review:;1990:;volume( 119 ):;issue: 007:;page 1714
    Author(s): Clark, John H. E.; Dembek, Scott R.
    Publisher: American Meteorological Society
    Abstract: The Catalina eddy that existed from 5 July to 12 July 1987 during FIRE (First ISSCP Regional Experiment) over offshore California is analyzed. There were two stages to the eddy's lifecycle. During the first, from 5 July ...
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    Mesospheric Heating Due to Convectively Excited Gravity Waves—A Case Study 

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 005:;page 990
    Author(s): Clark, John H. E.; Morone, Lauren Taylor
    Publisher: American Meteorological Society
    Abstract: A series of at least daily rocket soundings of the mesosphere at Wallops Island, Virginia (37°50?N, 75°29?W), in August and September 1976 reveal near simultaneity between rapid temperature rises and tropospheric convection ...
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