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    How Important Is the Spectral Ripening Effect in Stratiform Boundary Layer Clouds? Studies Using Simple Trajectory Analysis 

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 018:;page 2681
    Author(s): Wood, R.; Irons, S.; Jonas, P. R.
    Publisher: American Meteorological Society
    Abstract: Any population of cloud droplets forming on polydisperse condensation nuclei is thermodynamically unstable. There is no value of the supersaturation for which the growth rate of all the droplets is zero, so that if some ...
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    Analysis of an Air Motion System on a Light Aircraft for Boundary Layer Research 

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 004:;page 960
    Author(s): Wood, R.; Stromberg, I. M.; Jonas, P. R.; Mill, C. S.
    Publisher: American Meteorological Society
    Abstract: A system has been developed for use on a light aircraft for the measurement of the turbulent wind vector components that does not rely on the use of either an inertial navigation system (INS) or Doppler radar. The system ...
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    Observations of the Interaction between Cumulus Clouds and Warm Stratocumulus Clouds in the Marine Boundary Layer during ASTEX 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 016:;page 2902
    Author(s): Martin, G. M.; Johnson, D. W.; Rogers, D. P.; Jonas, P. R.; Minnis, P.; Hegg, D. A.
    Publisher: American Meteorological Society
    Abstract: Decoupling of the marine boundary layer beneath stratocumulus clouds and the formation of cumulus clouds at the top of a surface-based mixed layer (SML) have frequently been observed and modeled. When such cumulus clouds ...
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