Abstract
In a cold room collisions of two ice spheres having different growth modes were studied to examine ice production. The production of ice particles through this process was high, with a maximum rate more than 800 per collision at -16°C. This ice particle production mechanism is different from the Hallett-Mossop ice multiplication process and may help to explain the high concentrations of ice crystals observed in maritime winter cumuli. -Authors
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CITATION STYLE
Takahashi, T., Nagao, Y., & Kushiyama, Y. (1995). Possible high ice particle production during graupel-graupel collisions. Journal of the Atmospheric Sciences, 52(24), 4523–4527. https://doi.org/10.1175/1520-0469(1995)052<4523:PHIPPD>2.0.CO;2
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