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    The Marine Boundary Layer in the Vicinity of an Ocean Front 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 013:;page 2044
    Author(s): Rogers, David P.
    Publisher: American Meteorological Society
    Abstract: Aircraft observations obtained during the Frontal Air?Sea Interaction Experiment (FASINEX) are used to investigate the structure of the marine atmospheric boundary layer in the vicinity of an ocean front. A quasi-stationary ...
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    Detecting Ice Nuclei with a Continuous—Flow Diffusion Chamber-Some Exploratory Tests of Instrument Response 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 004:;page 1042
    Author(s): Rogers, David C.
    Publisher: American Meteorological Society
    Abstract: A few basic experiments were performed with artificial cloud condensation nuclei and ice-nucleating aerosols in a continuous-flow thermal gradient diffusion chamber to investigate the instrument's response. Brief pulses ...
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    The Future of the Global Weather Enterprise: Opportunities and Risks 

    Source: Bulletin of the American Meteorological Society:;2018:;volume 099:;issue 010:;page 2003
    Author(s): Thorpe, Alan; Rogers, David
    Publisher: American Meteorological Society
    Abstract: AbstractThe Global Weather Enterprise (GWE) encompasses the scientific research, technology, observations, modeling, forecasting, and forecast products that need to come together to provide accurate and reliable weather ...
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    Hailfalls and Hailstorm Feeder Clouds—an Alberta Case Study 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 023:;page 3533
    Author(s): Cheng, Lawrence; Rogers, David C.
    Publisher: American Meteorological Society
    Abstract: Observational evidence from an Alberta hailstorm was examined in an attempt to demonstrate the link between feeder clouds and hailfalls. Radar data, time resolved surface collections of hail, and cloud photographs from a ...
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    Turbulence Structure in Decoupled Marine Stratocumulus: A Case Study from the ASTEX Field Experiment 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 004:;page 598
    Author(s): Tjernström, Michael; Rogers, David P.
    Publisher: American Meteorological Society
    Abstract: The average and turbulence structure of two marine stratocumulus layers, from the Atlantic Stratocumulus Transition Experiment, are analyzed. These layers ware in adjacent air masses with different histories: one cloud ...
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    Numerical Simulations of the Response of the Marine Atmosphere to Ocean Forcing 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 005:;page 592
    Author(s): Koračin, Darko; Rogers, David P.
    Publisher: American Meteorological Society
    Abstract: The effect of a stable internal boundary layer (IBL) on the cloud-capped marine boundary layer is investigated using a one-dimensional second-order closure model. A stable IBL forms if there is a reversal in the surface ...
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    Radiative Transfer and Turbulence in the Cloud-topped Marine Atmospheric Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 016:;page 1473
    Author(s): Rogers, David P.; Korac̆in, Darko
    Publisher: American Meteorological Society
    Abstract: The effects of longwave and shortwave radiative heating on the coupling between stratocumulus clouds and the boundary layer is investigated using a one-dimensional second-moment turbulence-closure model. The decoupling of ...
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    Ice Crystal Production by Mountain Surfaces 

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 009:;page 1152
    Author(s): Rogers, David C.; Vali, Gabor
    Publisher: American Meteorological Society
    Abstract: Evidence is presented for a process of ice crystal generation in supercooled orographic clouds in contact with snow-covered mountain surfaces. Comparisons of the crystal concentrations at the surface with aircraft sampling ...
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    Freezing Nucleation Rates of Dilute Solution Droplets Measured between −30° and −40°C in Laboratory Simulations of Natural Clouds 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 009:;page 1056
    Author(s): DeMott, Paul J.; Rogers, David C.
    Publisher: American Meteorological Society
    Abstract: A 1.2 m3 continuous slow-expansion cloud chamber was used to simulate natural, liquid cloud formation on soluble cloud condensation nuclei (CCN). Droplet freezing was observed during continued simulated adiabatic ascent ...
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    On Mixing Processes in Continental Cumulus Clouds 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 001:;page 250
    Author(s): Gardiner, Barry A.; Rogers, David P.
    Publisher: American Meteorological Society
    Abstract: Results are presented from the 1981 Convective Cloud Precipitation Experiment (CCOPE). Aircraft data are analyzed from different flight levels within a convective cloud using the ?qQ mixing diagram (Paluch). Points on this ...
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