Depth-hoar growth rates near a rocky outcrop

Observations of slab-avalanche releases in alpine terrain have led to the hypothesis that rocky outcrops can influence the spatial distributions of temperature and heat flow in dry alpine snow covers and thus control the local distribution of depth hoar. We investigate the effects of terrain on crys...

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Main Authors: Arons, E. M., Colbeck, S. C., Gray, J. M N T
Format: Article in Journal/Newspaper
Language:English
Published: 1998
Subjects:
Online Access:https://research.manchester.ac.uk/en/publications/c0d0c187-4c70-4ae5-9667-87e65402cb07
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spelling ftumanchesterpub:oai:pure.atira.dk:publications/c0d0c187-4c70-4ae5-9667-87e65402cb07 2023-11-12T04:19:54+01:00 Depth-hoar growth rates near a rocky outcrop Arons, E. M. Colbeck, S. C. Gray, J. M N T 1998 https://research.manchester.ac.uk/en/publications/c0d0c187-4c70-4ae5-9667-87e65402cb07 eng eng info:eu-repo/semantics/restrictedAccess Arons , E M , Colbeck , S C & Gray , J M N T 1998 , ' Depth-hoar growth rates near a rocky outcrop ' , Journal of Glaciology , vol. 44 , no. 148 , pp. 477-484 . article 1998 ftumanchesterpub 2023-10-30T09:15:30Z Observations of slab-avalanche releases in alpine terrain have led to the hypothesis that rocky outcrops can influence the spatial distributions of temperature and heat flow in dry alpine snow covers and thus control the local distribution of depth hoar. We investigate the effects of terrain on crystal growth by using a two-dimensional finite-element model of heat flow coupled with a model of crystal growth from vapor. We used the model to examine the influence of snow properties, terrain geometry and snow depth on this phenomenon. The effect is stronger in the early winter than in the late winter, because the rock has then time to cool. In all cases, we found that depth-hoar growth occurs preferentially over the rock. This suggests that snow-pit investigations made over soil can be misleading if rocky outcrops are present. Article in Journal/Newspaper Journal of Glaciology The University of Manchester: Research Explorer
institution Open Polar
collection The University of Manchester: Research Explorer
op_collection_id ftumanchesterpub
language English
description Observations of slab-avalanche releases in alpine terrain have led to the hypothesis that rocky outcrops can influence the spatial distributions of temperature and heat flow in dry alpine snow covers and thus control the local distribution of depth hoar. We investigate the effects of terrain on crystal growth by using a two-dimensional finite-element model of heat flow coupled with a model of crystal growth from vapor. We used the model to examine the influence of snow properties, terrain geometry and snow depth on this phenomenon. The effect is stronger in the early winter than in the late winter, because the rock has then time to cool. In all cases, we found that depth-hoar growth occurs preferentially over the rock. This suggests that snow-pit investigations made over soil can be misleading if rocky outcrops are present.
format Article in Journal/Newspaper
author Arons, E. M.
Colbeck, S. C.
Gray, J. M N T
spellingShingle Arons, E. M.
Colbeck, S. C.
Gray, J. M N T
Depth-hoar growth rates near a rocky outcrop
author_facet Arons, E. M.
Colbeck, S. C.
Gray, J. M N T
author_sort Arons, E. M.
title Depth-hoar growth rates near a rocky outcrop
title_short Depth-hoar growth rates near a rocky outcrop
title_full Depth-hoar growth rates near a rocky outcrop
title_fullStr Depth-hoar growth rates near a rocky outcrop
title_full_unstemmed Depth-hoar growth rates near a rocky outcrop
title_sort depth-hoar growth rates near a rocky outcrop
publishDate 1998
url https://research.manchester.ac.uk/en/publications/c0d0c187-4c70-4ae5-9667-87e65402cb07
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Arons , E M , Colbeck , S C & Gray , J M N T 1998 , ' Depth-hoar growth rates near a rocky outcrop ' , Journal of Glaciology , vol. 44 , no. 148 , pp. 477-484 .
op_rights info:eu-repo/semantics/restrictedAccess
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