A Radar Profile of a Multi-year Pressure Ridge Fragment

. In May 1977, impulse radar was used to profile the thickness of an ice island and the first-year sea-ice near our camp site on Narwhal Island, Alaska. At this location, a small fragment of a multi-year pressure ridge was found with good access to the ridge crest. The impulse radar system was taken...

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Published in:ARCTIC
Main Author: Kovacs, Austin
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1978
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65692 2023-05-15T14:19:18+02:00 A Radar Profile of a Multi-year Pressure Ridge Fragment Kovacs, Austin 1978-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692/49606 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692 ARCTIC; Vol. 31 No. 1 (1978): March: 1–68; 59-62 1923-1245 0004-0843 Pressure ridges Ice islands Sea ice Radar Thickness Measurement Narwhal Island waters Alaska info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1978 ftunivcalgaryojs 2022-03-22T21:22:45Z . In May 1977, impulse radar was used to profile the thickness of an ice island and the first-year sea-ice near our camp site on Narwhal Island, Alaska. At this location, a small fragment of a multi-year pressure ridge was found with good access to the ridge crest. The impulse radar system was taken to the ridge so that it could be used to ascertain if thick multi-year ice could be measured and if the thickness of the ridge along the crest could be profiled. A cross-sectional profile of the ridge was not attempted, because the ice surface was buried under a thick layer of drift snow. The impulse radar profiling system consisted of an electronics console, a graphic recorder and an antenna. The system and its operational characteristics have been described in several publications. The radar antenna was pulled for a distance of 21 metres along the top of the ridge. . The signal information shown is the travel time of the radar impulse signal to and from the various reflecting surfaces. These include the surface of the ridge, internal block structure, and the irregular surface of the keel. . This report demonstrates the potential usefulness of impulse radar for determining the thickness of multi-year pressure ridges. . Article in Journal/Newspaper Arctic narwhal* Sea ice Alaska University of Calgary Journal Hosting Crest The ENVELOPE(-56.992,-56.992,-63.406,-63.406) ARCTIC 31 1
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Pressure ridges
Ice islands
Sea ice
Radar
Thickness
Measurement
Narwhal Island waters
Alaska
spellingShingle Pressure ridges
Ice islands
Sea ice
Radar
Thickness
Measurement
Narwhal Island waters
Alaska
Kovacs, Austin
A Radar Profile of a Multi-year Pressure Ridge Fragment
topic_facet Pressure ridges
Ice islands
Sea ice
Radar
Thickness
Measurement
Narwhal Island waters
Alaska
description . In May 1977, impulse radar was used to profile the thickness of an ice island and the first-year sea-ice near our camp site on Narwhal Island, Alaska. At this location, a small fragment of a multi-year pressure ridge was found with good access to the ridge crest. The impulse radar system was taken to the ridge so that it could be used to ascertain if thick multi-year ice could be measured and if the thickness of the ridge along the crest could be profiled. A cross-sectional profile of the ridge was not attempted, because the ice surface was buried under a thick layer of drift snow. The impulse radar profiling system consisted of an electronics console, a graphic recorder and an antenna. The system and its operational characteristics have been described in several publications. The radar antenna was pulled for a distance of 21 metres along the top of the ridge. . The signal information shown is the travel time of the radar impulse signal to and from the various reflecting surfaces. These include the surface of the ridge, internal block structure, and the irregular surface of the keel. . This report demonstrates the potential usefulness of impulse radar for determining the thickness of multi-year pressure ridges. .
format Article in Journal/Newspaper
author Kovacs, Austin
author_facet Kovacs, Austin
author_sort Kovacs, Austin
title A Radar Profile of a Multi-year Pressure Ridge Fragment
title_short A Radar Profile of a Multi-year Pressure Ridge Fragment
title_full A Radar Profile of a Multi-year Pressure Ridge Fragment
title_fullStr A Radar Profile of a Multi-year Pressure Ridge Fragment
title_full_unstemmed A Radar Profile of a Multi-year Pressure Ridge Fragment
title_sort radar profile of a multi-year pressure ridge fragment
publisher The Arctic Institute of North America
publishDate 1978
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692
long_lat ENVELOPE(-56.992,-56.992,-63.406,-63.406)
geographic Crest The
geographic_facet Crest The
genre Arctic
narwhal*
Sea ice
Alaska
genre_facet Arctic
narwhal*
Sea ice
Alaska
op_source ARCTIC; Vol. 31 No. 1 (1978): March: 1–68; 59-62
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692/49606
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65692
container_title ARCTIC
container_volume 31
container_issue 1
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