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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Language: | English |
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Cambridge University Press (CUP)
1953
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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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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 |
_version_ |
1792502115506061312 |