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A large piece of shore fast ice approximately 5 by 10 km broke free and drifted through Northumberland Strait on April 4 2003, failing against the piers of the Confederation Bridge. The ice had been surveyed shortly before its break-up and its thickness was about 1 m with many ridges of about 4 m th...

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Bibliographic Details
Main Authors: R. Frederking, I. Kubat, S. Prinsenberg
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2003
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.3486
http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.564.3486 2023-05-15T18:18:05+02:00 1 Reprinted from: R. Frederking I. Kubat S. Prinsenberg The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.3486 http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.3486 http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf text 2003 ftciteseerx 2016-01-08T12:11:28Z A large piece of shore fast ice approximately 5 by 10 km broke free and drifted through Northumberland Strait on April 4 2003, failing against the piers of the Confederation Bridge. The ice had been surveyed shortly before its break-up and its thickness was about 1 m with many ridges of about 4 m thick when averaged over a 20-m diameter. While the ice was quite thick, it was late in the season and thus soft resulting in the maximum force determined on the two piers only in the order of 2 MN. Hand held videos of the episode provided an overview of the ice failure processes observed. KEY WORDS: Ice forces; Structure response, Ice failure behaviour, Sea ice. Text Sea ice Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description A large piece of shore fast ice approximately 5 by 10 km broke free and drifted through Northumberland Strait on April 4 2003, failing against the piers of the Confederation Bridge. The ice had been surveyed shortly before its break-up and its thickness was about 1 m with many ridges of about 4 m thick when averaged over a 20-m diameter. While the ice was quite thick, it was late in the season and thus soft resulting in the maximum force determined on the two piers only in the order of 2 MN. Hand held videos of the episode provided an overview of the ice failure processes observed. KEY WORDS: Ice forces; Structure response, Ice failure behaviour, Sea ice.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author R. Frederking
I. Kubat
S. Prinsenberg
spellingShingle R. Frederking
I. Kubat
S. Prinsenberg
1 Reprinted from:
author_facet R. Frederking
I. Kubat
S. Prinsenberg
author_sort R. Frederking
title 1 Reprinted from:
title_short 1 Reprinted from:
title_full 1 Reprinted from:
title_fullStr 1 Reprinted from:
title_full_unstemmed 1 Reprinted from:
title_sort 1 reprinted from:
publishDate 2003
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.3486
http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf
genre Sea ice
genre_facet Sea ice
op_source http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.3486
http://www2.mar.dfo-mpo.gc.ca/science/ocean/seaice/publications/frederking01.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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