Estimating sea ice properties from wave observations in sea ice ...

The Marginal Ice Zone is a highly dynamic region where the atmosphere, ocean, waves and sea ice meet. Waves play a fundamental role in this coupled system, but progress in our understanding of wave-ice interactions is currently hindered by the lack of observations of sea ice properties in-situ. In t...

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Bibliographic Details
Main Authors: Voermans, J. J., Rabault, J., Marchenko, A., Nose, T., Waseda, T., Babanin, A. V.
Format: Report
Language:unknown
Published: arXiv 2023
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2305.06490
https://arxiv.org/abs/2305.06490
id ftdatacite:10.48550/arxiv.2305.06490
record_format openpolar
spelling ftdatacite:10.48550/arxiv.2305.06490 2023-06-11T04:16:30+02:00 Estimating sea ice properties from wave observations in sea ice ... Voermans, J. J. Rabault, J. Marchenko, A. Nose, T. Waseda, T. Babanin, A. V. 2023 https://dx.doi.org/10.48550/arxiv.2305.06490 https://arxiv.org/abs/2305.06490 unknown arXiv Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Geophysics physics.geo-ph Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences Preprint CreativeWork article Article 2023 ftdatacite https://doi.org/10.48550/arxiv.2305.06490 2023-06-01T11:34:27Z The Marginal Ice Zone is a highly dynamic region where the atmosphere, ocean, waves and sea ice meet. Waves play a fundamental role in this coupled system, but progress in our understanding of wave-ice interactions is currently hindered by the lack of observations of sea ice properties in-situ. In this study we aim to estimate the ice thickness and effective elastic modulus of sea ice passively using observations of waves in ice. Specifically, we use three low-cost geophones deployed in triangular formation with sides of about 200 m on fast ice. The focus here is on three major wave events recorded, each consisting of initial high frequency vibrations with a frequency at around 10 Hz, followed by low frequency dispersive waves within a frequency range of 0.08-0.28 Hz. Based on the phase speed of the initial high frequency vibrations, we estimate the purely elastic effective modulus to be 4-4.5 GPa. By comparing the arrival times of the dispersive low frequency wave events to the dispersion relationship of ... Report Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geophysics physics.geo-ph
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
spellingShingle Geophysics physics.geo-ph
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
Voermans, J. J.
Rabault, J.
Marchenko, A.
Nose, T.
Waseda, T.
Babanin, A. V.
Estimating sea ice properties from wave observations in sea ice ...
topic_facet Geophysics physics.geo-ph
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
description The Marginal Ice Zone is a highly dynamic region where the atmosphere, ocean, waves and sea ice meet. Waves play a fundamental role in this coupled system, but progress in our understanding of wave-ice interactions is currently hindered by the lack of observations of sea ice properties in-situ. In this study we aim to estimate the ice thickness and effective elastic modulus of sea ice passively using observations of waves in ice. Specifically, we use three low-cost geophones deployed in triangular formation with sides of about 200 m on fast ice. The focus here is on three major wave events recorded, each consisting of initial high frequency vibrations with a frequency at around 10 Hz, followed by low frequency dispersive waves within a frequency range of 0.08-0.28 Hz. Based on the phase speed of the initial high frequency vibrations, we estimate the purely elastic effective modulus to be 4-4.5 GPa. By comparing the arrival times of the dispersive low frequency wave events to the dispersion relationship of ...
format Report
author Voermans, J. J.
Rabault, J.
Marchenko, A.
Nose, T.
Waseda, T.
Babanin, A. V.
author_facet Voermans, J. J.
Rabault, J.
Marchenko, A.
Nose, T.
Waseda, T.
Babanin, A. V.
author_sort Voermans, J. J.
title Estimating sea ice properties from wave observations in sea ice ...
title_short Estimating sea ice properties from wave observations in sea ice ...
title_full Estimating sea ice properties from wave observations in sea ice ...
title_fullStr Estimating sea ice properties from wave observations in sea ice ...
title_full_unstemmed Estimating sea ice properties from wave observations in sea ice ...
title_sort estimating sea ice properties from wave observations in sea ice ...
publisher arXiv
publishDate 2023
url https://dx.doi.org/10.48550/arxiv.2305.06490
https://arxiv.org/abs/2305.06490
genre Sea ice
genre_facet Sea ice
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.48550/arxiv.2305.06490
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