论文信息 - The effect of fluid flow on the development of preferred orientations in sea ice: Laboratory experiments

The effect of fluid flow on the development of preferred orientations in sea ice: Laboratory experiments

Abstract Field evidence suggests that a strong crystallographic and growth alignment commonly observed in sea ice may form by the interaction of laminar fluid flow with the base of the growing ice cover. Laboratory experiments conducted in a cylindrical test basin support this hypothesis, and suggest that the observed alignment develops by the selective removal of brine at the ice-water interface.

Bernard Michel | E. Stander | E. Stander | B. Michel

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