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    Supersaturation Intermittency in Turbulent Clouds 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 020:;page 3452
    Author(s): Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: It is hypothesized that bursts of high supersaturation are produced in turbulent, convective clouds through interactions between cloud droplets and the small-scale structure of atmospheric turbulence. This hypothesis is ...
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    Supersaturation Fluctuations during the Early Stage of Cumulus Formation 

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 074 ):;issue: 004:;page 975
    Author(s): Siebert, Holger; Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: n time scales that are long compared to the phase relaxation time, a quasi-steady supersaturation sqs is expected to exist in clouds. On shorter time scales, however, turbulent fluctuations of temperature and water vapor ...
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    Visualizing Vapor Pressure: A Mechanical Demonstration of Liquid–Vapor Phase Equilibrium 

    Source: Bulletin of the American Meteorological Society:;2015:;volume( 097 ):;issue: 008:;page 1355
    Author(s): Lamb, Dennis; Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: ater phase transitions are central to climate and weather. Yet it is a common experience that the principles of phase equilibrium are challenging to understand and teach. A simple mechanical analogy has been developed to ...
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    Corrigendum 

    Source: Journal of the Atmospheric Sciences:;2017:;Volume( 074 ):;issue: 005:;page 1681
    Author(s): Kumar, Bipin; Schumacher, Jörg; Shaw, Raymond A.
    Publisher: American Meteorological Society
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    Homogeneous and Inhomogeneous Mixing in Cumulus Clouds: Dependence on Local Turbulence Structure 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 012:;page 3641
    Author(s): Lehmann, Katrin; Siebert, Holger; Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: The helicopter-borne instrument payload known as the Airborne Cloud Turbulence Observation System (ACTOS) was used to study the entrainment and mixing processes in shallow warm cumulus clouds. The characteristics of the ...
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    CORRIGENDUM 

    Source: Journal of the Atmospheric Sciences:;2015:;Volume( 072 ):;issue: 003:;page 1276
    Author(s): Kumar, Bipin; Schumacher, Jörg; Shaw, Raymond A.
    Publisher: American Meteorological Society
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    Fluctuations and Luck in Droplet Growth by Coalescence 

    Source: Bulletin of the American Meteorological Society:;2005:;volume( 086 ):;issue: 002:;page 235
    Author(s): Kostinski, Alexander B.; Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: After the initial rapid growth by condensation, further growth of a cloud droplet is punctuated by coalescence events. Such a growth process is essentially stochastic. Yet, computational approaches to this problem dominate ...
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    Supplement to: Fluctuations and Luck in Droplet Growth by Coalescence 

    Source: Bulletin of the American Meteorological Society:;2005:;volume( 086 ):;issue: 002:;page ES1
    Author(s): Kostinski, Alexander B.; Shaw, Raymond A.
    Publisher: American Meteorological Society
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    On the Use of Hot-Wire Anemometers for Turbulence Measurements in Clouds 

    Source: Journal of Atmospheric and Oceanic Technology:;2007:;volume( 024 ):;issue: 006:;page 980
    Author(s): Siebert, Holger; Lehmann, Katrin; Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: The use of a hot-wire anemometer for high-resolution turbulence measurements in a two-phase flow (e.g., atmospheric clouds) is discussed. Experiments in a small wind tunnel (diameter of 0.2 and 2 m in length) with a mean ...
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    Lagrangian Mixing Dynamics at the Cloudy–Clear Air Interface 

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 071 ):;issue: 007:;page 2564
    Author(s): Kumar, Bipin; Schumacher, Jörg; Shaw, Raymond A.
    Publisher: American Meteorological Society
    Abstract: he entrainment of clear air and its subsequent mixing with a filament of cloudy air, as occurs at the edge of a cloud, is studied in three-dimensional direct numerical simulations that combine the Eulerian description of ...
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    DSpace software copyright © 2002-2015  DuraSpace
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