Under Landfast Ice

The layer of water under landfast ice has unique oceanographic characteristics, as described in this review of recent assessment information for the central Alaskan Beaufort Sea coast. Water circulation is very slow usually near the lower threshold of current meters. Barometric storms cause infreque...

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Published in:ARCTIC
Main Author: Newbury, Thomas K.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1983
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65339 2023-05-15T14:19:16+02:00 Under Landfast Ice Newbury, Thomas K. 1983-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339/49253 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339 ARCTIC; Vol. 36 No. 4 (1983): December: 311–395; 328-340 1923-1245 0004-0843 Algae Breakup Fast ice Invertebrates Marine ecology Oceanography Predation Primary production (Biology) Sea ice ecology Winter ecology Wildlife habitat Alaskan Beaufort Sea info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1983 ftunivcalgaryojs 2022-03-22T21:22:25Z The layer of water under landfast ice has unique oceanographic characteristics, as described in this review of recent assessment information for the central Alaskan Beaufort Sea coast. Water circulation is very slow usually near the lower threshold of current meters. Barometric storms cause infrequent surges of water. The weak thermohaline-driven circulation is the reverse of that in ice-free estuaries. Water temperatures are always close to the slowly declining freezing point, and salinity gradually increases to high levels in bays because of flushing times of a month or more. Biological processes during the dark third of the year when there is no photosynthesis are dependent primarily on detritus and stored energy. Detritus is decomposed slowly by bacteria, and consumed by epibenthic invertebrates. Invertebrates and their main predators, fish, both reproduce under the ice cover. Food may limit biological activity in late winter, even in nearshore areas. Spring under-ice primary production totals possibly one-third of annual production with production of epontic algae attached to the bottom surface of the ice equalling only 5% of annual production. During breakup, river floods quickly flush under-ice areas; nearshore salinity drops to zero, and the wintertime thermohaline circulation is reversed. Year-to-year physical variations in the habitat cause the populations of three resident animals to vary up to sevenfold, but there are no regular cycles in abundance. Knowledge of these under-ice characteristics is important for understanding the Beaufort Sea coastal ecosystems, even for the relatively short open-water period.Key words: Arctic: Beaufort Sea, Alaska winter, coastal, landfast ice, under-ice, oceanography, food web Mots clés: Arctique, mer de Beaufort, Alaska, hiver, les côtes, glace attachée a la terre ferme, glace, au desous-blace, l'échelle de nourriture Article in Journal/Newspaper Arctic Arctic Arctique* Beaufort Sea Mer de Beaufort Sea ice Alaska University of Calgary Journal Hosting Arctic Mer de Beaufort ENVELOPE(-138.005,-138.005,69.500,69.500) ARCTIC 36 4
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Algae
Breakup
Fast ice
Invertebrates
Marine ecology
Oceanography
Predation
Primary production (Biology)
Sea ice ecology
Winter ecology
Wildlife habitat
Alaskan Beaufort Sea
spellingShingle Algae
Breakup
Fast ice
Invertebrates
Marine ecology
Oceanography
Predation
Primary production (Biology)
Sea ice ecology
Winter ecology
Wildlife habitat
Alaskan Beaufort Sea
Newbury, Thomas K.
Under Landfast Ice
topic_facet Algae
Breakup
Fast ice
Invertebrates
Marine ecology
Oceanography
Predation
Primary production (Biology)
Sea ice ecology
Winter ecology
Wildlife habitat
Alaskan Beaufort Sea
description The layer of water under landfast ice has unique oceanographic characteristics, as described in this review of recent assessment information for the central Alaskan Beaufort Sea coast. Water circulation is very slow usually near the lower threshold of current meters. Barometric storms cause infrequent surges of water. The weak thermohaline-driven circulation is the reverse of that in ice-free estuaries. Water temperatures are always close to the slowly declining freezing point, and salinity gradually increases to high levels in bays because of flushing times of a month or more. Biological processes during the dark third of the year when there is no photosynthesis are dependent primarily on detritus and stored energy. Detritus is decomposed slowly by bacteria, and consumed by epibenthic invertebrates. Invertebrates and their main predators, fish, both reproduce under the ice cover. Food may limit biological activity in late winter, even in nearshore areas. Spring under-ice primary production totals possibly one-third of annual production with production of epontic algae attached to the bottom surface of the ice equalling only 5% of annual production. During breakup, river floods quickly flush under-ice areas; nearshore salinity drops to zero, and the wintertime thermohaline circulation is reversed. Year-to-year physical variations in the habitat cause the populations of three resident animals to vary up to sevenfold, but there are no regular cycles in abundance. Knowledge of these under-ice characteristics is important for understanding the Beaufort Sea coastal ecosystems, even for the relatively short open-water period.Key words: Arctic: Beaufort Sea, Alaska winter, coastal, landfast ice, under-ice, oceanography, food web Mots clés: Arctique, mer de Beaufort, Alaska, hiver, les côtes, glace attachée a la terre ferme, glace, au desous-blace, l'échelle de nourriture
format Article in Journal/Newspaper
author Newbury, Thomas K.
author_facet Newbury, Thomas K.
author_sort Newbury, Thomas K.
title Under Landfast Ice
title_short Under Landfast Ice
title_full Under Landfast Ice
title_fullStr Under Landfast Ice
title_full_unstemmed Under Landfast Ice
title_sort under landfast ice
publisher The Arctic Institute of North America
publishDate 1983
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339
long_lat ENVELOPE(-138.005,-138.005,69.500,69.500)
geographic Arctic
Mer de Beaufort
geographic_facet Arctic
Mer de Beaufort
genre Arctic
Arctic
Arctique*
Beaufort Sea
Mer de Beaufort
Sea ice
Alaska
genre_facet Arctic
Arctic
Arctique*
Beaufort Sea
Mer de Beaufort
Sea ice
Alaska
op_source ARCTIC; Vol. 36 No. 4 (1983): December: 311–395; 328-340
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339/49253
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65339
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