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Frazil-Ice Nucleation by Mass-Exchange Processes at the Air-Water Interface
1977
Journal of Glaciology
AbstractThe physical requirements for proposed frazil-ice nucleation theories are reviewed in the light of recent observations on frazil-ice formation. It is concluded that spontaneous heterogeneous nucleation in a thin supercooled surface layer of water is not a viable mechanism for frazil-ice nucleation. Efforts to observe crystal multiplication by border ice have not been successful. The mass-exchange mechanism proposed by Osterkamp and others (1974) has been generalized to include
doi:10.3189/s0022143000215529
fatcat:cvplertwdnbfhfez4o6cz4ps5q