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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Published in:Natural Hazards and Earth System Sciences
Main Authors: Kurkina, O. E., Talipova, T. G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/nhess-11-981-2011
https://nhess.copernicus.org/articles/11/981/2011/
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spelling 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
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id 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
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