An investigation of the thermal conductivity of snow
Abstract Thermal conductivity of snow has been investigated experimentally using the thermal-probe method, which is a transient method of measurement. The measurements have been made over a wide range of snow density (for fresh and dense snow), for varying temperatures and for different conditions o...
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Cambridge University Press (CUP)
1999
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Online Access: | http://dx.doi.org/10.1017/s0022143000001842 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001842 |
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crcambridgeupr:10.1017/s0022143000001842 2024-04-07T07:53:41+00:00 An investigation of the thermal conductivity of snow Singh, A. K. 1999 http://dx.doi.org/10.1017/s0022143000001842 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001842 en eng Cambridge University Press (CUP) Journal of Glaciology volume 45, issue 150, page 346-351 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0022143000001842 2024-03-08T00:34:48Z Abstract Thermal conductivity of snow has been investigated experimentally using the thermal-probe method, which is a transient method of measurement. The measurements have been made over a wide range of snow density (for fresh and dense snow), for varying temperatures and for different conditions of water content, snow-grain type, etc., both in the field and in the laboratory. The results are presented along with detailed sample descriptions. Thermal conductivity of snow increases with density and water content. It also increases with temperature, and the effect is more pronounced for temperatures between –15° and 0°C. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 45 150 346 351 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Singh, A. K. An investigation of the thermal conductivity of snow |
topic_facet |
Earth-Surface Processes |
description |
Abstract Thermal conductivity of snow has been investigated experimentally using the thermal-probe method, which is a transient method of measurement. The measurements have been made over a wide range of snow density (for fresh and dense snow), for varying temperatures and for different conditions of water content, snow-grain type, etc., both in the field and in the laboratory. The results are presented along with detailed sample descriptions. Thermal conductivity of snow increases with density and water content. It also increases with temperature, and the effect is more pronounced for temperatures between –15° and 0°C. |
format |
Article in Journal/Newspaper |
author |
Singh, A. K. |
author_facet |
Singh, A. K. |
author_sort |
Singh, A. K. |
title |
An investigation of the thermal conductivity of snow |
title_short |
An investigation of the thermal conductivity of snow |
title_full |
An investigation of the thermal conductivity of snow |
title_fullStr |
An investigation of the thermal conductivity of snow |
title_full_unstemmed |
An investigation of the thermal conductivity of snow |
title_sort |
investigation of the thermal conductivity of snow |
publisher |
Cambridge University Press (CUP) |
publishDate |
1999 |
url |
http://dx.doi.org/10.1017/s0022143000001842 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001842 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 45, issue 150, page 346-351 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000001842 |
container_title |
Journal of Glaciology |
container_volume |
45 |
container_issue |
150 |
container_start_page |
346 |
op_container_end_page |
351 |
_version_ |
1795669771272847360 |