Item: Surface Hoar Growth from Valley Clouds
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Title: Surface Hoar Growth from Valley Clouds
Proceedings: Proceedings of the 2006 International Snow Science Workshop, Telluride, Colorado
Authors:
- Sam Colbeck [ Lyme, New Hampshire, USA ]
- Bruce Jamieson [ Dept. of Civil Engineering, Dept. of Geology and Geophysics, University of Calgary, Calgary, Canada ]
Date: 2006
Abstract: Avalanches release from buried surface hoar layers which form when stratus clouds extend across valleys on consecutive nights. Water vapor diffusion over distances of more than a meter is much too weak to account for the growth so non-diffusive movement in some form is necessary. The most likely mechanism for the formation of surface hoar is rapid deposition of vapor as the cloud thickens and moves up the snow slope. Since the time over which deposition could take place on any given night is short, successive nights are needed to produce a substantial deposit of hoar.
Object ID: issw-2006-001-006.pdf
Language of Article: English
Presenter(s): Unknown
Keywords: surface hoar, stratus cloud, snowpack stratigraphy, snow slab avalanches
Page Number(s): 1-6
Subjects: surface hoar valley clouds slab avalanche
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