We present the first clearly resolved observations of surfaces of growing and ablating hexagonal ice crystals using variable-pressure scanning electron microscopy. The ice surface develops trans-prismatic strands, separated from one another by distances of 5ĝ€"10 μm. The strands are present at a wide range of supersaturations, but are most pronounced at temperatures near the frost point. Pyramidal facets consistent with Miller-Bravais indices of 10 1 1, and possibly also 20 2 1, are associated with ice growth under these conditions. A molecular-dynamics model of a free-standing iceIh nanocolumn containing 8400 water molecules does not develop trans-prismatic strands, suggesting these features originate at larger spatial or temporal scales. The possible relevance of these surface features to cirrus ice is discussed. © 2010 Author(s).
CITATION STYLE
Pfalzgraff, W. C., Hulscher, R. M., & Neshyba, S. P. (2010). Scanning electron microscopy and molecular dynamics of surfaces of growing and ablating hexagonal ice crystals. Atmospheric Chemistry and Physics, 10(6), 2927–2935. https://doi.org/10.5194/acp-10-2927-2010
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