Rheological Properties of Low Density Snow
Widespread slab avalanches up to 1m deep often release immediately after the onset of rain on new snow. Measurements show that on first wetting the densification rate increases by about three orders of magnitude. It is likely that the initial burst of densification is a result of rapid structural ch...
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ftdtic:ADA366132 2023-05-15T16:37:47+02:00 Rheological Properties of Low Density Snow Conway, Howard WASHINGTON UNIV SEATTLE DEPT OF GEOPHYSICS 1998-12-09 text/html http://www.dtic.mil/docs/citations/ADA366132 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA366132 en eng http://www.dtic.mil/docs/citations/ADA366132 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *SNOW *RHEOLOGY AVALANCHES LOW DENSITY SLOPE STABILITY RAIN ON SNOW SNOW DENSIFICATION Text 1998 ftdtic 2016-02-20T02:24:05Z Widespread slab avalanches up to 1m deep often release immediately after the onset of rain on new snow. Measurements show that on first wetting the densification rate increases by about three orders of magnitude. It is likely that the initial burst of densification is a result of rapid structural changes and grain rearrangement. Abrupt changes in the mechanical properties are also likely but measurements show that only the upper 0.15m or less of the snowpack has been affected at the time of avalanching. We have not detected changes at the sliding layer. Results from an elastic slip-weakening model show the slab modulus may have a controlling influence on slope stability. It is evident that the mechanical properties of both the weak layer and the slab control slope stability. We have investigated the evolution of snow slope stability during storms by tracking the shear strength at a potential weak layer and the shear stress imposed by the weight of the overburden. Preliminary tests with the model are promising and State highway avalanche technicians plan to use it operationally at Snoqualmie Pass in the Washington Cascades during the coming winter. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost *SNOW *RHEOLOGY AVALANCHES LOW DENSITY SLOPE STABILITY RAIN ON SNOW SNOW DENSIFICATION |
spellingShingle |
Snow Ice and Permafrost *SNOW *RHEOLOGY AVALANCHES LOW DENSITY SLOPE STABILITY RAIN ON SNOW SNOW DENSIFICATION Conway, Howard Rheological Properties of Low Density Snow |
topic_facet |
Snow Ice and Permafrost *SNOW *RHEOLOGY AVALANCHES LOW DENSITY SLOPE STABILITY RAIN ON SNOW SNOW DENSIFICATION |
description |
Widespread slab avalanches up to 1m deep often release immediately after the onset of rain on new snow. Measurements show that on first wetting the densification rate increases by about three orders of magnitude. It is likely that the initial burst of densification is a result of rapid structural changes and grain rearrangement. Abrupt changes in the mechanical properties are also likely but measurements show that only the upper 0.15m or less of the snowpack has been affected at the time of avalanching. We have not detected changes at the sliding layer. Results from an elastic slip-weakening model show the slab modulus may have a controlling influence on slope stability. It is evident that the mechanical properties of both the weak layer and the slab control slope stability. We have investigated the evolution of snow slope stability during storms by tracking the shear strength at a potential weak layer and the shear stress imposed by the weight of the overburden. Preliminary tests with the model are promising and State highway avalanche technicians plan to use it operationally at Snoqualmie Pass in the Washington Cascades during the coming winter. |
author2 |
WASHINGTON UNIV SEATTLE DEPT OF GEOPHYSICS |
format |
Text |
author |
Conway, Howard |
author_facet |
Conway, Howard |
author_sort |
Conway, Howard |
title |
Rheological Properties of Low Density Snow |
title_short |
Rheological Properties of Low Density Snow |
title_full |
Rheological Properties of Low Density Snow |
title_fullStr |
Rheological Properties of Low Density Snow |
title_full_unstemmed |
Rheological Properties of Low Density Snow |
title_sort |
rheological properties of low density snow |
publishDate |
1998 |
url |
http://www.dtic.mil/docs/citations/ADA366132 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA366132 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA366132 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766028089635110912 |