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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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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 |
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English |
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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 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. |
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The Pennsylvania State University CiteSeerX Archives |
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R. Frederking I. Kubat S. Prinsenberg |
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R. Frederking I. Kubat S. Prinsenberg 1 Reprinted from: |
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R. Frederking I. Kubat S. Prinsenberg |
author_sort |
R. Frederking |
title |
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1 Reprinted from: |
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1 Reprinted from: |
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1 Reprinted from: |
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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 |
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Sea ice |
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Sea ice |
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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 |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766194325168848896 |