Density Variations in Alpine Snow
Abstract Stratigraphic studies of the annual snow layer in the Beartooth Mountains of south-western Montana and on Mount Logan in the St. Elias Range have disclosed a similiar distribution of at least one physical property of the snow pack in the two areas. The average density of the pack, obtained...
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Language: | English |
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Cambridge University Press (CUP)
1967
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Online Access: | http://dx.doi.org/10.1017/s0022143000019717 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019717 |
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crcambridgeupr:10.1017/s0022143000019717 2024-06-23T07:54:14+00:00 Density Variations in Alpine Snow Alford, Donald 1967 http://dx.doi.org/10.1017/s0022143000019717 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019717 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 46, page 495-503 ISSN 0022-1430 1727-5652 journal-article 1967 crcambridgeupr https://doi.org/10.1017/s0022143000019717 2024-06-12T04:05:06Z Abstract Stratigraphic studies of the annual snow layer in the Beartooth Mountains of south-western Montana and on Mount Logan in the St. Elias Range have disclosed a similiar distribution of at least one physical property of the snow pack in the two areas. The average density of the pack, obtained by integrating a series of measurements taken at 5–10 cm. vertical intervals over the total thickness of the annual layer, reaches a maximum value near a mid-point of the total elevation covered by each traverse and decreases linearly toward the elevation extremes. A preliminary hypothesis, relating the distribution of average snow-density values along slopes to a semi-stable zonation of near-surface air temperatures, is presented. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Mount Logan ENVELOPE(-140.405,-140.405,60.567,60.567) Journal of Glaciology 6 46 495 503 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract Stratigraphic studies of the annual snow layer in the Beartooth Mountains of south-western Montana and on Mount Logan in the St. Elias Range have disclosed a similiar distribution of at least one physical property of the snow pack in the two areas. The average density of the pack, obtained by integrating a series of measurements taken at 5–10 cm. vertical intervals over the total thickness of the annual layer, reaches a maximum value near a mid-point of the total elevation covered by each traverse and decreases linearly toward the elevation extremes. A preliminary hypothesis, relating the distribution of average snow-density values along slopes to a semi-stable zonation of near-surface air temperatures, is presented. |
format |
Article in Journal/Newspaper |
author |
Alford, Donald |
spellingShingle |
Alford, Donald Density Variations in Alpine Snow |
author_facet |
Alford, Donald |
author_sort |
Alford, Donald |
title |
Density Variations in Alpine Snow |
title_short |
Density Variations in Alpine Snow |
title_full |
Density Variations in Alpine Snow |
title_fullStr |
Density Variations in Alpine Snow |
title_full_unstemmed |
Density Variations in Alpine Snow |
title_sort |
density variations in alpine snow |
publisher |
Cambridge University Press (CUP) |
publishDate |
1967 |
url |
http://dx.doi.org/10.1017/s0022143000019717 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019717 |
long_lat |
ENVELOPE(-140.405,-140.405,60.567,60.567) |
geographic |
Mount Logan |
geographic_facet |
Mount Logan |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 6, issue 46, page 495-503 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000019717 |
container_title |
Journal of Glaciology |
container_volume |
6 |
container_issue |
46 |
container_start_page |
495 |
op_container_end_page |
503 |
_version_ |
1802646325226897408 |