On the excitation of resonant double Kelvin waves in the Barents Sea Opening

In the northern Barents Sea Opening (BSO) the K1 tidal energy is predominant in the diurnal tidal frequency band, suggesting the generation of a topographic wave with the K1 tidal frequency. Tidal energy of the K1 component becomes strong where bottom topography undulates in the BSO and the scale of...

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Published in:Polar Research
Main Authors: Kasajima, Yoshie, Marchenko, Aleksey
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2001
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2179
https://doi.org/10.3402/polar.v20i2.6523
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spelling ftjpolarres:oai:journals.openacademia.net:article/2179 2023-05-15T15:38:32+02:00 On the excitation of resonant double Kelvin waves in the Barents Sea Opening Kasajima, Yoshie Marchenko, Aleksey 2001-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2179 https://doi.org/10.3402/polar.v20i2.6523 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2179/5430 https://polarresearch.net/index.php/polar/article/view/2179 doi:10.3402/polar.v20i2.6523 Copyright (c) 2018 Polar Research Polar Research; Vol. 20 No. 2 (2001): Special issue: Proceedings of the H.U. Sverdrup Symposium; 241-248 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2001 ftjpolarres https://doi.org/10.3402/polar.v20i2.6523 2021-11-11T19:12:09Z In the northern Barents Sea Opening (BSO) the K1 tidal energy is predominant in the diurnal tidal frequency band, suggesting the generation of a topographic wave with the K1 tidal frequency. Tidal energy of the K1 component becomes strong where bottom topography undulates in the BSO and the scale of the undulation is close to the wavelength of the K1 wave. An analytical model is developed to investigate the energy enhancement mechanism of the tidally induced topographic wave due to a resonance between tidal current, a topographic wave and periodic topography. The wave excited by the resonance is identified as a resonant double Kelvin wave (DKW) and the significant K1 energy in the BSO could be due to the excitation of the resonant DKW. Article in Journal/Newspaper Barents Sea Polar Research Polar Research (E-Journal) Barents Sea Polar Research 20 2 241 248
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description In the northern Barents Sea Opening (BSO) the K1 tidal energy is predominant in the diurnal tidal frequency band, suggesting the generation of a topographic wave with the K1 tidal frequency. Tidal energy of the K1 component becomes strong where bottom topography undulates in the BSO and the scale of the undulation is close to the wavelength of the K1 wave. An analytical model is developed to investigate the energy enhancement mechanism of the tidally induced topographic wave due to a resonance between tidal current, a topographic wave and periodic topography. The wave excited by the resonance is identified as a resonant double Kelvin wave (DKW) and the significant K1 energy in the BSO could be due to the excitation of the resonant DKW.
format Article in Journal/Newspaper
author Kasajima, Yoshie
Marchenko, Aleksey
spellingShingle Kasajima, Yoshie
Marchenko, Aleksey
On the excitation of resonant double Kelvin waves in the Barents Sea Opening
author_facet Kasajima, Yoshie
Marchenko, Aleksey
author_sort Kasajima, Yoshie
title On the excitation of resonant double Kelvin waves in the Barents Sea Opening
title_short On the excitation of resonant double Kelvin waves in the Barents Sea Opening
title_full On the excitation of resonant double Kelvin waves in the Barents Sea Opening
title_fullStr On the excitation of resonant double Kelvin waves in the Barents Sea Opening
title_full_unstemmed On the excitation of resonant double Kelvin waves in the Barents Sea Opening
title_sort on the excitation of resonant double kelvin waves in the barents sea opening
publisher Norwegian Polar Institute
publishDate 2001
url https://polarresearch.net/index.php/polar/article/view/2179
https://doi.org/10.3402/polar.v20i2.6523
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
Polar Research
genre_facet Barents Sea
Polar Research
op_source Polar Research; Vol. 20 No. 2 (2001): Special issue: Proceedings of the H.U. Sverdrup Symposium; 241-248
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2179/5430
https://polarresearch.net/index.php/polar/article/view/2179
doi:10.3402/polar.v20i2.6523
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v20i2.6523
container_title Polar Research
container_volume 20
container_issue 2
container_start_page 241
op_container_end_page 248
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