Articles | Volume 15, issue 7
Atmos. Chem. Phys., 15, 3933–3956, 2015
Atmos. Chem. Phys., 15, 3933–3956, 2015
Research article
15 Apr 2015
Research article | 15 Apr 2015

Dimensions and aspect ratios of natural ice crystals

J. Um et al.

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Cited articles

Arnott, W. P., Dong, Y. Y., and Hallet, J.: Role of small ice crystals in radiative properties of cirrus: A case study, FIRE II, November 22, 1991, J. Geophys. Res., 99, 1371–81, 1994.
Auer, A. H. and Veal, D. L.: The dimension of ice crystals in natural clouds, J. Atmos. Sci., 27, 919–926, 1970.
aufm Kampe, H. J., Weickmann, H. K., and Kelly, J. J.: The influence of temperature on the shape of ice crystals growing at water saturation, J. Meteorol., 8, 168–174, 1951.
Bacon, N. J., Baker, M. B., and Swanson, B. D.: Initial stages in the morphological evolution of vapour-grown ice crystals: A laboratory investigation, Q. J. Roy. Meteor. Soc., 129, 1903–1927, 2003.
Bailey, M. P. and Hallett, J.: Nucleation effects on the habit of vapour grown ice crystals from −18 to −42 \degree C, Q. J. Roy. Meteor. Soc., 128, 1461–1483, 2002.
Short summary
Dimensions of ice crystals increased with an increase in temperature and the L-W relationships of crystals with a given L depended heavily on temperature, whereas the aspect ratio depended only weakly on temperature. The relative frequency of occurrence of plates was much larger in anvil clouds compared to that of columnar crystals (i.e., columns and bullet rosettes), whereas the relative occurrence frequency of columnar crystals was much larger in non-anvil clouds.
Final-revised paper