Abstract
Two anomalies are described which arise in the kernel for stochastic droplet collection when it is specified by the formula of Scott and Chen for the linear collision efficiency y(R,r) and by the formula of Wobus et al. for the droplet terminal velocity V(R). It is pointed out that if accurate values for y(R,r) are to be obtained for a given droplet pair by interpolation using data for specific droplet pairs, then for large droplet radii it is desirable that these data be tabulated for 2- mu m intervales of radius R. It is shown that if the difference in terminal velocities of two droplets is computed from a formula approximating V(R) and composed of various functions V*(R) applicable over adjoining domains of R, then it is necessary that these functions be constructed so that the formula and its derivatives, at least up to second order, are everywhere continuous. An improved formula for V(R) satisfying this criterion is described.
Cite
CITATION STYLE
Long, A. B., & Manton, M. J. (1974). ON THE EVALUATION OF THE COLLECTION KERNEL FOR THE COALESCENCE OF WATER DROPLETS. Journal of the Atmospheric Sciences, 31(4), 1053–1057. https://doi.org/10.1175/1520-0469(1974)031<1053:OTEOTC>2.0.CO;2
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