Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea)
The generation of huge amplitude internal waves by the barotropic tide in the Barents Sea at high latitudes is examined using the numerical model of the Euler 2-D equations for incompressible stratified fluid. The area considered is located between the Spitsbergen (Svalbard) Island and the Franz-Vic...
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Online Access: | https://doi.org/10.5194/nhess-11-981-2011 https://nhess.copernicus.org/articles/11/981/2011/ |
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ftcopernicus:oai:publications.copernicus.org:nhess8904 2023-05-15T15:38:32+02:00 Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) Kurkina, O. E. Talipova, T. G. 2018-09-27 application/pdf https://doi.org/10.5194/nhess-11-981-2011 https://nhess.copernicus.org/articles/11/981/2011/ eng eng doi:10.5194/nhess-11-981-2011 https://nhess.copernicus.org/articles/11/981/2011/ eISSN: 1684-9981 Text 2018 ftcopernicus https://doi.org/10.5194/nhess-11-981-2011 2020-07-20T16:26:09Z The generation of huge amplitude internal waves by the barotropic tide in the Barents Sea at high latitudes is examined using the numerical model of the Euler 2-D equations for incompressible stratified fluid. The area considered is located between the Spitsbergen (Svalbard) Island and the Franz-Victoria Trough with a cross-section of 350 km length. There are two underwater hills about 100–150 m high on the background depth of about 300 m. It is shown that intensive nonlinear internal waves with amplitudes up to 50 m and lengths of about 6–12 km are generated in this zone. The total height of such waves is huge and they must be considered as a significant factor of the environment in this basin. Text Barents Sea Svalbard Spitsbergen Copernicus Publications: E-Journals Svalbard Barents Sea Natural Hazards and Earth System Sciences 11 3 981 986 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The generation of huge amplitude internal waves by the barotropic tide in the Barents Sea at high latitudes is examined using the numerical model of the Euler 2-D equations for incompressible stratified fluid. The area considered is located between the Spitsbergen (Svalbard) Island and the Franz-Victoria Trough with a cross-section of 350 km length. There are two underwater hills about 100–150 m high on the background depth of about 300 m. It is shown that intensive nonlinear internal waves with amplitudes up to 50 m and lengths of about 6–12 km are generated in this zone. The total height of such waves is huge and they must be considered as a significant factor of the environment in this basin. |
format |
Text |
author |
Kurkina, O. E. Talipova, T. G. |
spellingShingle |
Kurkina, O. E. Talipova, T. G. Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) |
author_facet |
Kurkina, O. E. Talipova, T. G. |
author_sort |
Kurkina, O. E. |
title |
Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) |
title_short |
Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) |
title_full |
Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) |
title_fullStr |
Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) |
title_full_unstemmed |
Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea) |
title_sort |
huge internal waves in the vicinity of the spitsbergen island (barents sea) |
publishDate |
2018 |
url |
https://doi.org/10.5194/nhess-11-981-2011 https://nhess.copernicus.org/articles/11/981/2011/ |
geographic |
Svalbard Barents Sea |
geographic_facet |
Svalbard Barents Sea |
genre |
Barents Sea Svalbard Spitsbergen |
genre_facet |
Barents Sea Svalbard Spitsbergen |
op_source |
eISSN: 1684-9981 |
op_relation |
doi:10.5194/nhess-11-981-2011 https://nhess.copernicus.org/articles/11/981/2011/ |
op_doi |
https://doi.org/10.5194/nhess-11-981-2011 |
container_title |
Natural Hazards and Earth System Sciences |
container_volume |
11 |
container_issue |
3 |
container_start_page |
981 |
op_container_end_page |
986 |
_version_ |
1766369537350959104 |