Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake
Making use of limited ground temperature measurements in the neighbourhood of a small shallow lake near Inuvik, N.W.T., it was possible with the help of an electronic computer to estimate the entire thermal regime under and about the lake. The results indicated a completely unfrozen zone of roughly...
Published in: | Canadian Geotechnical Journal |
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Language: | English |
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Canadian Science Publishing
1964
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Online Access: | http://dx.doi.org/10.1139/t64-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/t64-009 |
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crcansciencepubl:10.1139/t64-009 2024-09-09T19:48:24+00:00 Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake Brown, W G Johnston, G H Brown, R. J. E 1964 http://dx.doi.org/10.1139/t64-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/t64-009 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 1, issue 3, page 147-154 ISSN 0008-3674 1208-6010 journal-article 1964 crcansciencepubl https://doi.org/10.1139/t64-009 2024-06-20T04:11:55Z Making use of limited ground temperature measurements in the neighbourhood of a small shallow lake near Inuvik, N.W.T., it was possible with the help of an electronic computer to estimate the entire thermal regime under and about the lake. The results indicated a completely unfrozen zone of roughly hour-glass shape directly under the lake. Field borings under the lake and adjacent to it supported this theoretical finding. Article in Journal/Newspaper Inuvik permafrost Canadian Science Publishing Inuvik ENVELOPE(-133.610,-133.610,68.341,68.341) Canadian Geotechnical Journal 1 3 147 154 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
Making use of limited ground temperature measurements in the neighbourhood of a small shallow lake near Inuvik, N.W.T., it was possible with the help of an electronic computer to estimate the entire thermal regime under and about the lake. The results indicated a completely unfrozen zone of roughly hour-glass shape directly under the lake. Field borings under the lake and adjacent to it supported this theoretical finding. |
format |
Article in Journal/Newspaper |
author |
Brown, W G Johnston, G H Brown, R. J. E |
spellingShingle |
Brown, W G Johnston, G H Brown, R. J. E Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake |
author_facet |
Brown, W G Johnston, G H Brown, R. J. E |
author_sort |
Brown, W G |
title |
Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake |
title_short |
Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake |
title_full |
Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake |
title_fullStr |
Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake |
title_full_unstemmed |
Comparison of Observed and Calculated Ground Temperatures with Permafrost Distribution under a Northern Lake |
title_sort |
comparison of observed and calculated ground temperatures with permafrost distribution under a northern lake |
publisher |
Canadian Science Publishing |
publishDate |
1964 |
url |
http://dx.doi.org/10.1139/t64-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/t64-009 |
long_lat |
ENVELOPE(-133.610,-133.610,68.341,68.341) |
geographic |
Inuvik |
geographic_facet |
Inuvik |
genre |
Inuvik permafrost |
genre_facet |
Inuvik permafrost |
op_source |
Canadian Geotechnical Journal volume 1, issue 3, page 147-154 ISSN 0008-3674 1208-6010 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/t64-009 |
container_title |
Canadian Geotechnical Journal |
container_volume |
1 |
container_issue |
3 |
container_start_page |
147 |
op_container_end_page |
154 |
_version_ |
1809917685650161664 |