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    Effects of Variable Droplet Growth Histories on Droplet Size Distributions. Part I: Theory 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 010:;page 1301
    Author(s): Cooper, William A.
    Publisher: American Meteorological Society
    Abstract: A theoretical framework is developed that permits estimation of the effects of fluctuating supersaturation on the development of cloud droplet size spectra. The studies focus on the role of turbulent fluctuations in vertical ...
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    Effects of Coincidence on Measurements with a Forward Scattering Spectrometer Probe 

    Source: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006:;page 823
    Author(s): Cooper, William A.
    Publisher: American Meteorological Society
    Abstract: A PMS Forward Scattering Spectrometer Probe (FSSP) may fail to detect a droplet that enters the illuminated volume in coincidence with another droplet, or such a coincident pair may be assigned an erroneous size. This ...
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    Reply 

    Source: Journal of Climate and Applied Meteorology:;1985:;Volume( 024 ):;Issue: 011:;page 1275
    Author(s): Cooper, William A.
    Publisher: American Meteorological Society
    Abstract: tract
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    A Possible Mechanism for Contact Nucleation 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 007:;page 1832
    Author(s): Cooper, William A.
    Publisher: American Meteorological Society
    Abstract: A contact nucleation mechanism is suggested, by which ice embryos formed on a nucleus in vapor are able to nucleate supercooled water on contact. Using conventional nucleation theory, the activity of a contact nucleus is ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 012:;page 2373
    Author(s): Cooper, William A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Comment on “The Collection Kernel for Two Falling Cloud Drops Subjected to Random Perturbations in a Turbulent Air Flow: A Stochastic Model” 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 008:;page 1165
    Author(s): Cooper, William A.; Baumgardner, Darrel
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    The Origin of Ice in Mountain Cap Clouds 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 006:;page 1244
    Author(s): Cooper, William A.; Vali, Gabor
    Publisher: American Meteorological Society
    Abstract: Ice crystal development in relatively simple layer clouds was studied using airborne instrumentation. The patterns in the development of ice in those clouds suggest that the ice originates in association with the initial ...
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    Effects of Airflow Trajectories Around Aircraft on Measurements of Scalar Fluxes 

    Source: Journal of Atmospheric and Oceanic Technology:;1991:;volume( 008 ):;issue: 001:;page 66
    Author(s): Cooper, William A.; Rogers, Diana
    Publisher: American Meteorological Society
    Abstract: Potential-flow calculations of the airflow around two research aircraft are used to estimate the effect of flow distortion on measured fluxes of sensible heat and water vapor. From the calculated flow patterns, flow-distortion ...
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    Variability of the Supersaturation in Cumulus Clouds 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 011:;page 1651
    Author(s): Politovich, Marcia K.; Cooper, William A.
    Publisher: American Meteorological Society
    Abstract: The quasi-steady supersaturation in cumulus clouds from the Cooperative Convective Precipitation Experiment of 1981 are calculated from measurements of vertical wind, cloud droplet size, temperature and pressure. Mean ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 017:;page 2752
    Author(s): Cooper, William A.; Politovich, Marcia K.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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