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...
Main Authors: | , , , , , |
---|---|
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 |
_version_ |
1768374830783004672 |