ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA
For the engineering design of underwater pipelines and communication cables in freezing seas, reliable estimates of the frequency and penetration depth of ice-keel scour on the seabed and shoreface are required. Underestimation of ice gouging intensity on the seabed can lead to the infrastructure da...
Published in: | GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY |
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Lomonosov Moscow State University
2013
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Online Access: | https://doi.org/10.24057/2071-9388-2013-6-3-21-37 https://doaj.org/article/fd92bc92ace6480eaee3c3ee0a075ecf |
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ftdoajarticles:oai:doaj.org/article:fd92bc92ace6480eaee3c3ee0a075ecf 2023-05-15T15:05:49+02:00 ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA Stanislav Ogorodov Vasiliy Arkhipov Osip Kokin Aleksey Marchenko Paul Overduin Donald Forbes 2013-09-01T00:00:00Z https://doi.org/10.24057/2071-9388-2013-6-3-21-37 https://doaj.org/article/fd92bc92ace6480eaee3c3ee0a075ecf EN eng Lomonosov Moscow State University https://ges.rgo.ru/jour/article/view/138 https://doaj.org/toc/2071-9388 https://doaj.org/toc/2542-1565 2071-9388 2542-1565 doi:10.24057/2071-9388-2013-6-3-21-37 https://doaj.org/article/fd92bc92ace6480eaee3c3ee0a075ecf Geography, Environment, Sustainability, Vol 6, Iss 3, Pp 21-37 (2013) kara sea arctic coastal dynamics geotechnical safety sea ice ice ridges ice gouging bottom topography the intensity of ice influence zoning Geography (General) G1-922 article 2013 ftdoajarticles https://doi.org/10.24057/2071-9388-2013-6-3-21-37 2023-03-19T01:40:21Z For the engineering design of underwater pipelines and communication cables in freezing seas, reliable estimates of the frequency and penetration depth of ice-keel scour on the seabed and shoreface are required. Underestimation of ice gouging intensity on the seabed can lead to the infrastructure damage, while overestimation leading to excessive burial depth raises the cost of construction. Here we present results from recent studies of ice gouge morphology in Baydaratskaya Bay, Kara Sea. The direct impact of ice gouging by floes on the seabed and shores is described, generalized and systematized: the depth of the gouges varies from the first centimeters up to 2 m; the most intensive ice gouging is observed near the fast ice rim, due to the maximum impact executed by ice ridges frozen into large floe. We propose a zonation of Baydaratskaya Bay based on the types of ice formation and the intensity of ice impacts on the coasts and sea floor. Article in Journal/Newspaper Arctic Baydaratskaya bay Kara Sea Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Kara Sea GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 6 3 21 37 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
kara sea arctic coastal dynamics geotechnical safety sea ice ice ridges ice gouging bottom topography the intensity of ice influence zoning Geography (General) G1-922 |
spellingShingle |
kara sea arctic coastal dynamics geotechnical safety sea ice ice ridges ice gouging bottom topography the intensity of ice influence zoning Geography (General) G1-922 Stanislav Ogorodov Vasiliy Arkhipov Osip Kokin Aleksey Marchenko Paul Overduin Donald Forbes ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA |
topic_facet |
kara sea arctic coastal dynamics geotechnical safety sea ice ice ridges ice gouging bottom topography the intensity of ice influence zoning Geography (General) G1-922 |
description |
For the engineering design of underwater pipelines and communication cables in freezing seas, reliable estimates of the frequency and penetration depth of ice-keel scour on the seabed and shoreface are required. Underestimation of ice gouging intensity on the seabed can lead to the infrastructure damage, while overestimation leading to excessive burial depth raises the cost of construction. Here we present results from recent studies of ice gouge morphology in Baydaratskaya Bay, Kara Sea. The direct impact of ice gouging by floes on the seabed and shores is described, generalized and systematized: the depth of the gouges varies from the first centimeters up to 2 m; the most intensive ice gouging is observed near the fast ice rim, due to the maximum impact executed by ice ridges frozen into large floe. We propose a zonation of Baydaratskaya Bay based on the types of ice formation and the intensity of ice impacts on the coasts and sea floor. |
format |
Article in Journal/Newspaper |
author |
Stanislav Ogorodov Vasiliy Arkhipov Osip Kokin Aleksey Marchenko Paul Overduin Donald Forbes |
author_facet |
Stanislav Ogorodov Vasiliy Arkhipov Osip Kokin Aleksey Marchenko Paul Overduin Donald Forbes |
author_sort |
Stanislav Ogorodov |
title |
ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA |
title_short |
ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA |
title_full |
ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA |
title_fullStr |
ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA |
title_full_unstemmed |
ICE EFFECT ON COAST AND SEABED IN BAYDARATSKAYA BAY, KARA SEA |
title_sort |
ice effect on coast and seabed in baydaratskaya bay, kara sea |
publisher |
Lomonosov Moscow State University |
publishDate |
2013 |
url |
https://doi.org/10.24057/2071-9388-2013-6-3-21-37 https://doaj.org/article/fd92bc92ace6480eaee3c3ee0a075ecf |
geographic |
Arctic Kara Sea |
geographic_facet |
Arctic Kara Sea |
genre |
Arctic Baydaratskaya bay Kara Sea Sea ice |
genre_facet |
Arctic Baydaratskaya bay Kara Sea Sea ice |
op_source |
Geography, Environment, Sustainability, Vol 6, Iss 3, Pp 21-37 (2013) |
op_relation |
https://ges.rgo.ru/jour/article/view/138 https://doaj.org/toc/2071-9388 https://doaj.org/toc/2542-1565 2071-9388 2542-1565 doi:10.24057/2071-9388-2013-6-3-21-37 https://doaj.org/article/fd92bc92ace6480eaee3c3ee0a075ecf |
op_doi |
https://doi.org/10.24057/2071-9388-2013-6-3-21-37 |
container_title |
GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY |
container_volume |
6 |
container_issue |
3 |
container_start_page |
21 |
op_container_end_page |
37 |
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1766337464040947712 |