Crossref journal-article
Wiley
Quarterly Journal of the Royal Meteorological Society (311)
Abstract

AbstractIt is shown theoretically that the rate of nucleation of the ice phase in supercooled water changes very rapidly with temperature in the neighbourhood of −40°C. Thus, in chilling a supercooled water cloud below this temperature one would expect to observe a rapid increase in the number of ice crystals which appear as the temperature falls. This is verified by observations made in a cold chamber. The different critical temperatures for the spontaneous appearance of ice crystals quoted by Schaefer (−39°) and the Oxford workers (−41°C) probably arise as the result of differences in the experimental conditions. It is tentatively suggested that the parts of mother‐of‐pearl clouds showing iridescence at temperatures around −80°C consist of spheres of ‘glassy’ ice, which may eventually crystallize spontaneously to form ice crystals towards the leeward edges of the cloud.

Bibliography

Mason, B. J. (1952). The spontaneous crystallization of supercooled water. Quarterly Journal of the Royal Meteorological Society, 78(335), 22–27. Portico.

Authors 1
  1. B. J. Mason (first)
References 19 Referenced 39
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Dates
Type When
Created 18 years, 6 months ago (Feb. 2, 2007, 7:05 p.m.)
Deposited 1 year, 9 months ago (Nov. 4, 2023, 4:56 p.m.)
Indexed 1 year, 6 months ago (Feb. 8, 2024, 2:22 p.m.)
Issued 73 years, 7 months ago (Jan. 1, 1952)
Published 73 years, 7 months ago (Jan. 1, 1952)
Published Online 18 years, 8 months ago (Dec. 14, 2006)
Published Print 73 years, 7 months ago (Jan. 1, 1952)
Funders 0

None

@article{Mason_1952, title={The spontaneous crystallization of supercooled water}, volume={78}, ISSN={1477-870X}, url={http://dx.doi.org/10.1002/qj.49707833503}, DOI={10.1002/qj.49707833503}, number={335}, journal={Quarterly Journal of the Royal Meteorological Society}, publisher={Wiley}, author={Mason, B. J.}, year={1952}, month=jan, pages={22–27} }