Notes on the Oceanography of d'Iberville Fiord
The oceanography of a small arctic fiord has been studied over a period of three years. The shallow water structure is determined by convection in the fiord, as is shown by temperature-time series and budget studies. The fiord contains temperature inversions at shallow depths, which have been presen...
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The Arctic Institute of North America
1973
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ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65970 2023-05-15T14:19:19+02:00 Notes on the Oceanography of d'Iberville Fiord Lake, R.A. Walker, E.R. 1973-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65970 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65970/49884 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65970 ARCTIC; Vol. 26 No. 3 (1973): September: 177–268; 222-229 1923-1245 0004-0843 Active layer info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1973 ftunivcalgaryojs 2022-03-22T21:22:59Z The oceanography of a small arctic fiord has been studied over a period of three years. The shallow water structure is determined by convection in the fiord, as is shown by temperature-time series and budget studies. The fiord contains temperature inversions at shallow depths, which have been present in observations over several years. The deeper water structure is determined by the sill across the fiord mouth and similar sills in Nansen Sound that restrict free access at depth of water layers from the Arctic Ocean. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Nansen Sound University of Calgary Journal Hosting Arctic Arctic Ocean d'Iberville Fiord ENVELOPE(-78.997,-78.997,80.569,80.569) Nansen Sound ENVELOPE(-90.584,-90.584,81.002,81.002) ARCTIC 26 3 |
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University of Calgary Journal Hosting |
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English |
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Active layer |
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Active layer Lake, R.A. Walker, E.R. Notes on the Oceanography of d'Iberville Fiord |
topic_facet |
Active layer |
description |
The oceanography of a small arctic fiord has been studied over a period of three years. The shallow water structure is determined by convection in the fiord, as is shown by temperature-time series and budget studies. The fiord contains temperature inversions at shallow depths, which have been present in observations over several years. The deeper water structure is determined by the sill across the fiord mouth and similar sills in Nansen Sound that restrict free access at depth of water layers from the Arctic Ocean. |
format |
Article in Journal/Newspaper |
author |
Lake, R.A. Walker, E.R. |
author_facet |
Lake, R.A. Walker, E.R. |
author_sort |
Lake, R.A. |
title |
Notes on the Oceanography of d'Iberville Fiord |
title_short |
Notes on the Oceanography of d'Iberville Fiord |
title_full |
Notes on the Oceanography of d'Iberville Fiord |
title_fullStr |
Notes on the Oceanography of d'Iberville Fiord |
title_full_unstemmed |
Notes on the Oceanography of d'Iberville Fiord |
title_sort |
notes on the oceanography of d'iberville fiord |
publisher |
The Arctic Institute of North America |
publishDate |
1973 |
url |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65970 |
long_lat |
ENVELOPE(-78.997,-78.997,80.569,80.569) ENVELOPE(-90.584,-90.584,81.002,81.002) |
geographic |
Arctic Arctic Ocean d'Iberville Fiord Nansen Sound |
geographic_facet |
Arctic Arctic Ocean d'Iberville Fiord Nansen Sound |
genre |
Arctic Arctic Arctic Ocean Nansen Sound |
genre_facet |
Arctic Arctic Arctic Ocean Nansen Sound |
op_source |
ARCTIC; Vol. 26 No. 3 (1973): September: 177–268; 222-229 1923-1245 0004-0843 |
op_relation |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65970/49884 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65970 |
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ARCTIC |
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