Internal Waves under Ice Cover

Colloque avec actes et comité de lecture. Internationale. International audience A theoretical model for propagation of internal waves under an ice cover is developed. The sea water is considered to be inviscid, non-rotating, and incompressible and the Brunt–Väisälä frequency is supposed to be const...

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Main Author: MUZYLEV, Sergey
Other Authors: Association Française de Mécanique
Format: Conference Object
Language:English
Published: HAL CCSD 2007
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-03359876
https://hal.archives-ouvertes.fr/hal-03359876/document
https://hal.archives-ouvertes.fr/hal-03359876/file/bitstream_22231.pdf
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record_format openpolar
spelling ftccsdartic:oai:HAL:hal-03359876v1 2023-05-15T15:04:14+02:00 Internal Waves under Ice Cover MUZYLEV, Sergey Association Française de Mécanique Grenoble, France 2007-08-27 https://hal.archives-ouvertes.fr/hal-03359876 https://hal.archives-ouvertes.fr/hal-03359876/document https://hal.archives-ouvertes.fr/hal-03359876/file/bitstream_22231.pdf en eng HAL CCSD AFM, Maison de la Mécanique, 39/41 rue Louis Blanc - 92400 Courbevoie hal-03359876 https://hal.archives-ouvertes.fr/hal-03359876 https://hal.archives-ouvertes.fr/hal-03359876/document https://hal.archives-ouvertes.fr/hal-03359876/file/bitstream_22231.pdf info:eu-repo/semantics/OpenAccess CFM 2007 - 18ème Congrès Français de Mécanique https://hal.archives-ouvertes.fr/hal-03359876 CFM 2007 - 18ème Congrès Français de Mécanique, Aug 2007, Grenoble, France internal waves ice deflections Vaisala frequency [PHYS.MECA]Physics [physics]/Mechanics [physics] info:eu-repo/semantics/conferenceObject Conference papers 2007 ftccsdartic 2021-10-02T22:21:59Z Colloque avec actes et comité de lecture. Internationale. International audience A theoretical model for propagation of internal waves under an ice cover is developed. The sea water is considered to be inviscid, non-rotating, and incompressible and the Brunt–Väisälä frequency is supposed to be constant. The ice is considered of uniform thickness, with constant values of Young's modulus, Poisson's ratio, density and compressive stress in the ice. The boundary conditions are such that the normal velocity at the bottom is zero and, at the undersurface of the ice, the linearized kinematical and dynamic boundary conditions are satisfied. We present and analyze explicit solutions for the internal waves under the ice cover and the dispersion equations. It is shown that when the frequency is near, but smaller than the Brunt–Väisälä frequency the ice deflections can be considerable. The theoretical results are compared with experimental data for the Arctic regions. Conference Object Arctic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic internal waves
ice deflections
Vaisala frequency
[PHYS.MECA]Physics [physics]/Mechanics [physics]
spellingShingle internal waves
ice deflections
Vaisala frequency
[PHYS.MECA]Physics [physics]/Mechanics [physics]
MUZYLEV, Sergey
Internal Waves under Ice Cover
topic_facet internal waves
ice deflections
Vaisala frequency
[PHYS.MECA]Physics [physics]/Mechanics [physics]
description Colloque avec actes et comité de lecture. Internationale. International audience A theoretical model for propagation of internal waves under an ice cover is developed. The sea water is considered to be inviscid, non-rotating, and incompressible and the Brunt–Väisälä frequency is supposed to be constant. The ice is considered of uniform thickness, with constant values of Young's modulus, Poisson's ratio, density and compressive stress in the ice. The boundary conditions are such that the normal velocity at the bottom is zero and, at the undersurface of the ice, the linearized kinematical and dynamic boundary conditions are satisfied. We present and analyze explicit solutions for the internal waves under the ice cover and the dispersion equations. It is shown that when the frequency is near, but smaller than the Brunt–Väisälä frequency the ice deflections can be considerable. The theoretical results are compared with experimental data for the Arctic regions.
author2 Association Française de Mécanique
format Conference Object
author MUZYLEV, Sergey
author_facet MUZYLEV, Sergey
author_sort MUZYLEV, Sergey
title Internal Waves under Ice Cover
title_short Internal Waves under Ice Cover
title_full Internal Waves under Ice Cover
title_fullStr Internal Waves under Ice Cover
title_full_unstemmed Internal Waves under Ice Cover
title_sort internal waves under ice cover
publisher HAL CCSD
publishDate 2007
url https://hal.archives-ouvertes.fr/hal-03359876
https://hal.archives-ouvertes.fr/hal-03359876/document
https://hal.archives-ouvertes.fr/hal-03359876/file/bitstream_22231.pdf
op_coverage Grenoble, France
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source CFM 2007 - 18ème Congrès Français de Mécanique
https://hal.archives-ouvertes.fr/hal-03359876
CFM 2007 - 18ème Congrès Français de Mécanique, Aug 2007, Grenoble, France
op_relation hal-03359876
https://hal.archives-ouvertes.fr/hal-03359876
https://hal.archives-ouvertes.fr/hal-03359876/document
https://hal.archives-ouvertes.fr/hal-03359876/file/bitstream_22231.pdf
op_rights info:eu-repo/semantics/OpenAccess
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