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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Published in:Journal of Glaciology
Main Author: Alford, Donald
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1967
Subjects:
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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spelling 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
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