Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska

Four large grounded multi-year shear ridge formations were found in the grounded ice subzone of the fast ice zone near the Harrison Bay/Prudhoe Bay area of Alaska. A 166-m-long cross section of one of these formations was obtained by leveling and sonar measurements. These measurements revealed that...

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Bibliographic Details
Main Author: Kovacs,Austin
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1976
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA031352
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA031352
id ftdtic:ADA031352
record_format openpolar
spelling ftdtic:ADA031352 2023-05-15T15:40:32+02:00 Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska Kovacs,Austin COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1976-09 text/html http://www.dtic.mil/docs/citations/ADA031352 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA031352 en eng http://www.dtic.mil/docs/citations/ADA031352 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *ICE *SEA ICE *BEAUFORT SEA *ICE ISLANDS *ICE REPORTING DENSITY TEMPERATURE THICKNESS COASTAL REGIONS ALASKA SURFACE ROUGHNESS ICE FORMATION METEOROLOGICAL RADAR SALINITY SONAR BRINES SIDE LOOKING RADAR CORE SAMPLING PACK ICE *Harrison Bay Prudhoe Bay Text 1976 ftdtic 2016-02-20T11:38:03Z Four large grounded multi-year shear ridge formations were found in the grounded ice subzone of the fast ice zone near the Harrison Bay/Prudhoe Bay area of Alaska. A 166-m-long cross section of one of these formations was obtained by leveling and sonar measurements. These measurements revealed that the maximum ridge height was 12.6 m and that the formation was grounded in 17-18 m of water. The salinity, temperature, brine volume and density of the ice were determined on samples obtained by coring. The physical characteristics of the formations as observed in satellite, SLAR and aerial imagery indicate that these formations have not moved between the time of their formation in the fall of 1974 and August of 1976. Evidence of significant aeolian debris discoloring the ice is discussed. Text Beaufort Sea Ice permafrost Prudhoe Bay Sea ice Alaska Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ICE
*SEA ICE
*BEAUFORT SEA
*ICE ISLANDS
*ICE REPORTING
DENSITY
TEMPERATURE
THICKNESS
COASTAL REGIONS
ALASKA
SURFACE ROUGHNESS
ICE FORMATION
METEOROLOGICAL RADAR
SALINITY
SONAR
BRINES
SIDE LOOKING RADAR
CORE SAMPLING
PACK ICE
*Harrison Bay
Prudhoe Bay
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ICE
*SEA ICE
*BEAUFORT SEA
*ICE ISLANDS
*ICE REPORTING
DENSITY
TEMPERATURE
THICKNESS
COASTAL REGIONS
ALASKA
SURFACE ROUGHNESS
ICE FORMATION
METEOROLOGICAL RADAR
SALINITY
SONAR
BRINES
SIDE LOOKING RADAR
CORE SAMPLING
PACK ICE
*Harrison Bay
Prudhoe Bay
Kovacs,Austin
Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ICE
*SEA ICE
*BEAUFORT SEA
*ICE ISLANDS
*ICE REPORTING
DENSITY
TEMPERATURE
THICKNESS
COASTAL REGIONS
ALASKA
SURFACE ROUGHNESS
ICE FORMATION
METEOROLOGICAL RADAR
SALINITY
SONAR
BRINES
SIDE LOOKING RADAR
CORE SAMPLING
PACK ICE
*Harrison Bay
Prudhoe Bay
description Four large grounded multi-year shear ridge formations were found in the grounded ice subzone of the fast ice zone near the Harrison Bay/Prudhoe Bay area of Alaska. A 166-m-long cross section of one of these formations was obtained by leveling and sonar measurements. These measurements revealed that the maximum ridge height was 12.6 m and that the formation was grounded in 17-18 m of water. The salinity, temperature, brine volume and density of the ice were determined on samples obtained by coring. The physical characteristics of the formations as observed in satellite, SLAR and aerial imagery indicate that these formations have not moved between the time of their formation in the fall of 1974 and August of 1976. Evidence of significant aeolian debris discoloring the ice is discussed.
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
format Text
author Kovacs,Austin
author_facet Kovacs,Austin
author_sort Kovacs,Austin
title Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska
title_short Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska
title_full Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska
title_fullStr Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska
title_full_unstemmed Grounded Ice in the Fast Ice Zone along the Beaufort Seacoast of Alaska
title_sort grounded ice in the fast ice zone along the beaufort seacoast of alaska
publishDate 1976
url http://www.dtic.mil/docs/citations/ADA031352
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA031352
genre Beaufort Sea
Ice
permafrost
Prudhoe Bay
Sea ice
Alaska
genre_facet Beaufort Sea
Ice
permafrost
Prudhoe Bay
Sea ice
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA031352
op_rights APPROVED FOR PUBLIC RELEASE
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