Drift of Sea Ice Ridges in the Pechora Sea

The drift of sea ice ridges and hits on an offshore structure with dimensions 200 m by 200 m have been studied for the Dolginskoye oil field in the Pechora Sea. The calculations were made with the computer program ICEBERG. The mean drift speed of the ice ridges was found to be 0·21 m/s with a maximu...

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Published in:Journal of Navigation
Main Authors: Johannessen, Kenneth, Gudmestad, Ove Tobias, Løset, Sveinung
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2001
Subjects:
Online Access:https://doi.org/10.1017/s0373463300001144
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0373463300001144
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author Johannessen, Kenneth
Gudmestad, Ove Tobias
Løset, Sveinung
author_facet Johannessen, Kenneth
Gudmestad, Ove Tobias
Løset, Sveinung
author_sort Johannessen, Kenneth
collection Cambridge University Press
container_issue 1
container_start_page 81
container_title Journal of Navigation
container_volume 54
description The drift of sea ice ridges and hits on an offshore structure with dimensions 200 m by 200 m have been studied for the Dolginskoye oil field in the Pechora Sea. The calculations were made with the computer program ICEBERG. The mean drift speed of the ice ridges was found to be 0·21 m/s with a maximum speed of 0·89 m/s. The expected number of hits per year was calculated to be 737. It was assumed that a total number of 133000 sea ice ridges would be produced in (or have entered) the Pechora Sea per year. Under the same assumption, the expected number of ridges entering a safety zone around a platform of 1852 m by 1852 m was found to be 5649. However, due to uncertainties concerning the population of ridges, their shapes, sizes, drag coefficients and tidal action, the results should be used with care and only considered as indicative. The ridge drift pattern was predominantly to the northeast in the winter months. A structure located at Dolginskoye will most probably be exposed to sea ice ridges that are formed in the area around Khodovarihka.
format Article in Journal/Newspaper
genre Pechora
Pechora Sea
Sea ice
genre_facet Pechora
Pechora Sea
Sea ice
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op_container_end_page 96
op_doi https://doi.org/10.1017/s0373463300001144
op_rights https://www.cambridge.org/core/terms
op_source Journal of Navigation
volume 54, issue 1, page 81-96
ISSN 0373-4633 1469-7785
publishDate 2001
publisher Cambridge University Press (CUP)
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spelling crcambridgeupr:10.1017/s0373463300001144 2025-05-04T14:34:16+00:00 Drift of Sea Ice Ridges in the Pechora Sea Johannessen, Kenneth Gudmestad, Ove Tobias Løset, Sveinung 2001 https://doi.org/10.1017/s0373463300001144 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0373463300001144 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Navigation volume 54, issue 1, page 81-96 ISSN 0373-4633 1469-7785 journal-article 2001 crcambridgeupr https://doi.org/10.1017/s0373463300001144 2025-04-08T13:12:25Z The drift of sea ice ridges and hits on an offshore structure with dimensions 200 m by 200 m have been studied for the Dolginskoye oil field in the Pechora Sea. The calculations were made with the computer program ICEBERG. The mean drift speed of the ice ridges was found to be 0·21 m/s with a maximum speed of 0·89 m/s. The expected number of hits per year was calculated to be 737. It was assumed that a total number of 133000 sea ice ridges would be produced in (or have entered) the Pechora Sea per year. Under the same assumption, the expected number of ridges entering a safety zone around a platform of 1852 m by 1852 m was found to be 5649. However, due to uncertainties concerning the population of ridges, their shapes, sizes, drag coefficients and tidal action, the results should be used with care and only considered as indicative. The ridge drift pattern was predominantly to the northeast in the winter months. A structure located at Dolginskoye will most probably be exposed to sea ice ridges that are formed in the area around Khodovarihka. Article in Journal/Newspaper Pechora Pechora Sea Sea ice Cambridge University Press Journal of Navigation 54 1 81 96
spellingShingle Johannessen, Kenneth
Gudmestad, Ove Tobias
Løset, Sveinung
Drift of Sea Ice Ridges in the Pechora Sea
title Drift of Sea Ice Ridges in the Pechora Sea
title_full Drift of Sea Ice Ridges in the Pechora Sea
title_fullStr Drift of Sea Ice Ridges in the Pechora Sea
title_full_unstemmed Drift of Sea Ice Ridges in the Pechora Sea
title_short Drift of Sea Ice Ridges in the Pechora Sea
title_sort drift of sea ice ridges in the pechora sea
url https://doi.org/10.1017/s0373463300001144
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0373463300001144