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...
Published in: | Geophysical Research Letters |
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Online Access: | https://doi.org/10.1029/2023GL105243 https://doaj.org/article/d4aee4a3e73f4c0c9906c2a4f0e769ed |
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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 |
_version_ |
1810429830702825472 |