Ice crystal morphology and growth rates at low supersaturations and high temperatures
- 1 May 1983
- journal article
- conference paper
- Published by AIP Publishing in Journal of Applied Physics
- Vol. 54 (5) , 2677-2682
- https://doi.org/10.1063/1.332290
Abstract
At an excess vapor density (supersaturation of about 10−4) adjacent to the ice crystal surface of 5–6×10−10 g/cc, there is a transition between the highly faceted kinetic growth form and the rounded equilibrium form at temperatures above –6 °C. At lower temperatures there is a transition in the equilibrium form to hexagonal prisms because of a reduction in the disordered surface layer. The growth rate of ice crystals from the vapor is analyzed by a simple model which accounts for vapor flow and surface processes separately. The conditions for highly temperature sensitive growth are identified from the model.This publication has 12 references indexed in Scilit:
- An overview of seasonal snow metamorphismReviews of Geophysics, 1982
- Growth kinetics of ice from the vapour phase and its growth formsJournal of Crystal Growth, 1982
- Experimental observation of the surface roughening transition in vapor phase growthJournal of Crystal Growth, 1977
- Snow Crystal Habit at Small Excesses of Vapor Density over Ice SaturationJournal of the Atmospheric Sciences, 1974
- The Mechanism of Ice Crystal Growth and Habit FormationJournal of the Atmospheric Sciences, 1974
- Les surfaces non-singulières sur la forme d'équilibre du naphtalèneJournal of Crystal Growth, 1972
- The surface morphology of epitaxial siliconJournal of Crystal Growth, 1971
- On the appearance and growth of non-singular crystal surfacesJournal of Crystal Growth, 1968
- Theory of crystal growth and interface motion in crystalline materialsActa Metallurgica, 1960
- The growth of crystals and the equilibrium structure of their surfacesPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1951