The Effect of Accumulation on Temperatures within A Snowfield

Abstract The wave of cold temperature, which begins to propagate into a snow field during the winter, may be considerably enhanced by the thermal blanketing of snow accumulating on the surface. This effect is discussed theoretically by means of calculations based on the mathematical theory of the co...

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Published in:Journal of Glaciology
Main Author: Benfield, A. E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1953
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000025429
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025429
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spelling crcambridgeupr:10.1017/s0022143000025429 2024-03-03T08:46:09+00:00 The Effect of Accumulation on Temperatures within A Snowfield Benfield, A. E. 1953 http://dx.doi.org/10.1017/s0022143000025429 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025429 en eng Cambridge University Press (CUP) Journal of Glaciology volume 2, issue 14, page 250-254 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1953 crcambridgeupr https://doi.org/10.1017/s0022143000025429 2024-02-08T08:42:50Z Abstract The wave of cold temperature, which begins to propagate into a snow field during the winter, may be considerably enhanced by the thermal blanketing of snow accumulating on the surface. This effect is discussed theoretically by means of calculations based on the mathematical theory of the conduction of heat in solids. The results of these calculations show that for an assumed steady velocity of accumulation at the rate of 4 meters/year or 8 meters/year, the winter cold wave should assume significantly larger proportions than in the absence of accumulation. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 2 14 250 254
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Benfield, A. E.
The Effect of Accumulation on Temperatures within A Snowfield
topic_facet Earth-Surface Processes
description Abstract The wave of cold temperature, which begins to propagate into a snow field during the winter, may be considerably enhanced by the thermal blanketing of snow accumulating on the surface. This effect is discussed theoretically by means of calculations based on the mathematical theory of the conduction of heat in solids. The results of these calculations show that for an assumed steady velocity of accumulation at the rate of 4 meters/year or 8 meters/year, the winter cold wave should assume significantly larger proportions than in the absence of accumulation.
format Article in Journal/Newspaper
author Benfield, A. E.
author_facet Benfield, A. E.
author_sort Benfield, A. E.
title The Effect of Accumulation on Temperatures within A Snowfield
title_short The Effect of Accumulation on Temperatures within A Snowfield
title_full The Effect of Accumulation on Temperatures within A Snowfield
title_fullStr The Effect of Accumulation on Temperatures within A Snowfield
title_full_unstemmed The Effect of Accumulation on Temperatures within A Snowfield
title_sort effect of accumulation on temperatures within a snowfield
publisher Cambridge University Press (CUP)
publishDate 1953
url http://dx.doi.org/10.1017/s0022143000025429
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025429
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 2, issue 14, page 250-254
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000025429
container_title Journal of Glaciology
container_volume 2
container_issue 14
container_start_page 250
op_container_end_page 254
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