Heat exchange and sea ice growth in Arctic Canada.
Stefan's equation for ice accretion has been modified to take into account the affects of snow depth and density. For regions in the Canadian Arctic the modified equation, when applied in the presence of a light snow cover with climatic estimates of heat loss, gave a satisfactory explanation of...
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McGill University
1966
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ftcanadathes:oai:collectionscanada.gc.ca:QMM.47600 2023-05-15T14:43:14+02:00 Heat exchange and sea ice growth in Arctic Canada. Leahey, D. M. Orvig, S. (Supervisor) Master of Science (Department of Meteorology) 1966 application/pdf http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=47600 en eng McGill University alephsysno: 000455982 proquestno: AAIMK00331 Theses scanned by UMI/ProQuest. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=47600 All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. Ice -- Canada Meteorology. Electronic Thesis or Dissertation 1966 ftcanadathes 2014-02-16T01:10:28Z Stefan's equation for ice accretion has been modified to take into account the affects of snow depth and density. For regions in the Canadian Arctic the modified equation, when applied in the presence of a light snow cover with climatic estimates of heat loss, gave a satisfactory explanation of the observed ice growth (correlation coefficient = .99). [.] Thesis Arctic Sea ice Theses Canada/Thèses Canada (Library and Archives Canada) Arctic Canada |
institution |
Open Polar |
collection |
Theses Canada/Thèses Canada (Library and Archives Canada) |
op_collection_id |
ftcanadathes |
language |
English |
topic |
Ice -- Canada Meteorology. |
spellingShingle |
Ice -- Canada Meteorology. Leahey, D. M. Heat exchange and sea ice growth in Arctic Canada. |
topic_facet |
Ice -- Canada Meteorology. |
description |
Stefan's equation for ice accretion has been modified to take into account the affects of snow depth and density. For regions in the Canadian Arctic the modified equation, when applied in the presence of a light snow cover with climatic estimates of heat loss, gave a satisfactory explanation of the observed ice growth (correlation coefficient = .99). [.] |
author2 |
Orvig, S. (Supervisor) |
format |
Thesis |
author |
Leahey, D. M. |
author_facet |
Leahey, D. M. |
author_sort |
Leahey, D. M. |
title |
Heat exchange and sea ice growth in Arctic Canada. |
title_short |
Heat exchange and sea ice growth in Arctic Canada. |
title_full |
Heat exchange and sea ice growth in Arctic Canada. |
title_fullStr |
Heat exchange and sea ice growth in Arctic Canada. |
title_full_unstemmed |
Heat exchange and sea ice growth in Arctic Canada. |
title_sort |
heat exchange and sea ice growth in arctic canada. |
publisher |
McGill University |
publishDate |
1966 |
url |
http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=47600 |
op_coverage |
Master of Science (Department of Meteorology) |
geographic |
Arctic Canada |
geographic_facet |
Arctic Canada |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_relation |
alephsysno: 000455982 proquestno: AAIMK00331 Theses scanned by UMI/ProQuest. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=47600 |
op_rights |
All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
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1766314913856225280 |