Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables

Abstract The attenuation of ocean surface waves during seasonal ice cover is an important control on the evolution of Arctic coastlines. The spatial and temporal variations in this process have been challenging to resolve with conventional sampling using sparse arrays of moorings or buoys. We demons...

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Published in:Geophysical Research Letters
Main Authors: Madison M. Smith, Jim Thomson, Michael G. Baker, Robert E. Abbott, Jake Davis
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
DAS
Online Access:https://doi.org/10.1029/2023GL105243
https://doaj.org/article/d4aee4a3e73f4c0c9906c2a4f0e769ed
id ftdoajarticles:oai:doaj.org/article:d4aee4a3e73f4c0c9906c2a4f0e769ed
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spelling ftdoajarticles:oai:doaj.org/article:d4aee4a3e73f4c0c9906c2a4f0e769ed 2024-09-15T17:53:46+00:00 Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables Madison M. Smith Jim Thomson Michael G. Baker Robert E. Abbott Jake Davis 2023-10-01T00:00:00Z https://doi.org/10.1029/2023GL105243 https://doaj.org/article/d4aee4a3e73f4c0c9906c2a4f0e769ed EN eng Wiley https://doi.org/10.1029/2023GL105243 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL105243 https://doaj.org/article/d4aee4a3e73f4c0c9906c2a4f0e769ed Geophysical Research Letters, Vol 50, Iss 20, Pp n/a-n/a (2023) sea ice waves Arctic Ocean coastal shelves DAS Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL105243 2024-08-05T17:49:23Z Abstract The attenuation of ocean surface waves during seasonal ice cover is an important control on the evolution of Arctic coastlines. The spatial and temporal variations in this process have been challenging to resolve with conventional sampling using sparse arrays of moorings or buoys. We demonstrate a novel method for persistent observation of wave‐ice interactions using distributed acoustic sensing (DAS) along existing seafloor fiber optic telecommunications cables. DAS measurements span a 36‐km cross‐shore cable on the Beaufort Shelf from Oliktok Point, Alaska. DAS optical sensing of fiber strain‐rate provides a proxy for seafloor pressure, which we calibrate with wave buoy measurements during the ice‐free season (August 2022). We apply this calibration during the ice formation season (November 2021) to obtain unprecedented resolution of variable wave attenuation rates in new, partial ice cover. The location and strength of wave attenuation serve as proxies for ice coverage and thickness, especially during rapidly evolving events. Article in Journal/Newspaper Arctic Ocean Sea ice Alaska Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 20
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic sea ice
waves
Arctic Ocean
coastal shelves
DAS
Geophysics. Cosmic physics
QC801-809
spellingShingle sea ice
waves
Arctic Ocean
coastal shelves
DAS
Geophysics. Cosmic physics
QC801-809
Madison M. Smith
Jim Thomson
Michael G. Baker
Robert E. Abbott
Jake Davis
Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables
topic_facet sea ice
waves
Arctic Ocean
coastal shelves
DAS
Geophysics. Cosmic physics
QC801-809
description Abstract The attenuation of ocean surface waves during seasonal ice cover is an important control on the evolution of Arctic coastlines. The spatial and temporal variations in this process have been challenging to resolve with conventional sampling using sparse arrays of moorings or buoys. We demonstrate a novel method for persistent observation of wave‐ice interactions using distributed acoustic sensing (DAS) along existing seafloor fiber optic telecommunications cables. DAS measurements span a 36‐km cross‐shore cable on the Beaufort Shelf from Oliktok Point, Alaska. DAS optical sensing of fiber strain‐rate provides a proxy for seafloor pressure, which we calibrate with wave buoy measurements during the ice‐free season (August 2022). We apply this calibration during the ice formation season (November 2021) to obtain unprecedented resolution of variable wave attenuation rates in new, partial ice cover. The location and strength of wave attenuation serve as proxies for ice coverage and thickness, especially during rapidly evolving events.
format Article in Journal/Newspaper
author Madison M. Smith
Jim Thomson
Michael G. Baker
Robert E. Abbott
Jake Davis
author_facet Madison M. Smith
Jim Thomson
Michael G. Baker
Robert E. Abbott
Jake Davis
author_sort Madison M. Smith
title Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables
title_short Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables
title_full Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables
title_fullStr Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables
title_full_unstemmed Observations of Ocean Surface Wave Attenuation in Sea Ice Using Seafloor Cables
title_sort observations of ocean surface wave attenuation in sea ice using seafloor cables
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL105243
https://doaj.org/article/d4aee4a3e73f4c0c9906c2a4f0e769ed
genre Arctic Ocean
Sea ice
Alaska
genre_facet Arctic Ocean
Sea ice
Alaska
op_source Geophysical Research Letters, Vol 50, Iss 20, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL105243
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL105243
https://doaj.org/article/d4aee4a3e73f4c0c9906c2a4f0e769ed
op_doi https://doi.org/10.1029/2023GL105243
container_title Geophysical Research Letters
container_volume 50
container_issue 20
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