Abstract
A theory for canting has been developed from the response of raindrops to shear produced by homogeneous, isotropic turbulence. The model predicts small canting angles, with the tangent of the angle having a Gaussian probability distribution about a mean value of zero. -from Authors
Cite
CITATION STYLE
APA
Beard, K. V., & Jameson, A. R. (1983). Raindrop canting. Journal of the Atmospheric Sciences, 40(2), 448–454. https://doi.org/10.1175/1520-0469(1983)040<0448:RC>2.0.CO;2
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