Oceanographic conditions during 1973 in Russell Fjord, Alaska

Russell Fjord appears to be in the process of being dammed and isolated from marine influence by the advancing Hubbard Glacier. This study was initiated to understand the present circulation of the fjord and to provide a basis for comparison in the event that closure should occur. Observations made...

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Main Authors: Reeburgh, WS, Muench, RD, Cooney, RT
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 1976
Subjects:
Online Access:https://escholarship.org/uc/item/1jp7h1n1
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spelling ftcdlib:oai:escholarship.org:ark:/13030/qt1jp7h1n1 2023-06-18T03:40:42+02:00 Oceanographic conditions during 1973 in Russell Fjord, Alaska Reeburgh, WS Muench, RD Cooney, RT 129 - 145 1976-03-01 application/pdf https://escholarship.org/uc/item/1jp7h1n1 unknown eScholarship, University of California qt1jp7h1n1 https://escholarship.org/uc/item/1jp7h1n1 CC-BY Estuarine Coastal and Shelf Science, vol 4, iss 2 Marine Biology & Hydrobiology article 1976 ftcdlib 2023-06-05T18:02:17Z Russell Fjord appears to be in the process of being dammed and isolated from marine influence by the advancing Hubbard Glacier. This study was initiated to understand the present circulation of the fjord and to provide a basis for comparison in the event that closure should occur. Observations made during 1973 indicate that the deep water is continuously renewed by near-surface source water added over the sill. 'NO' (Broecker, 1974) appears to be useful in tracing these additions. The probable consequences of glacial damming are considered. © 1976. Article in Journal/Newspaper glacier Alaska University of California: eScholarship Hubbard Glacier ENVELOPE(-139.379,-139.379,60.344,60.344)
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Marine Biology & Hydrobiology
spellingShingle Marine Biology & Hydrobiology
Reeburgh, WS
Muench, RD
Cooney, RT
Oceanographic conditions during 1973 in Russell Fjord, Alaska
topic_facet Marine Biology & Hydrobiology
description Russell Fjord appears to be in the process of being dammed and isolated from marine influence by the advancing Hubbard Glacier. This study was initiated to understand the present circulation of the fjord and to provide a basis for comparison in the event that closure should occur. Observations made during 1973 indicate that the deep water is continuously renewed by near-surface source water added over the sill. 'NO' (Broecker, 1974) appears to be useful in tracing these additions. The probable consequences of glacial damming are considered. © 1976.
format Article in Journal/Newspaper
author Reeburgh, WS
Muench, RD
Cooney, RT
author_facet Reeburgh, WS
Muench, RD
Cooney, RT
author_sort Reeburgh, WS
title Oceanographic conditions during 1973 in Russell Fjord, Alaska
title_short Oceanographic conditions during 1973 in Russell Fjord, Alaska
title_full Oceanographic conditions during 1973 in Russell Fjord, Alaska
title_fullStr Oceanographic conditions during 1973 in Russell Fjord, Alaska
title_full_unstemmed Oceanographic conditions during 1973 in Russell Fjord, Alaska
title_sort oceanographic conditions during 1973 in russell fjord, alaska
publisher eScholarship, University of California
publishDate 1976
url https://escholarship.org/uc/item/1jp7h1n1
op_coverage 129 - 145
long_lat ENVELOPE(-139.379,-139.379,60.344,60.344)
geographic Hubbard Glacier
geographic_facet Hubbard Glacier
genre glacier
Alaska
genre_facet glacier
Alaska
op_source Estuarine Coastal and Shelf Science, vol 4, iss 2
op_relation qt1jp7h1n1
https://escholarship.org/uc/item/1jp7h1n1
op_rights CC-BY
_version_ 1769005948350758912