Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation

Air bubble penetration depths are investigated with a bottom‐mounted echosounder at a seabed observatory in northern Norway. We compare a 1‐year time series of observed bubble depth against modeled and estimated turbulent kinetic energy flux from breaking waves as well as wind speed and sea state. W...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Strand, Kjersti Opstad, Breivik, Øyvind, Pedersen, Geir, Vikebø, Frode Bendiksen, Sundby, Svein, Christensen, Kai Håkon
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:http://hdl.handle.net/10852/79319
http://urn.nb.no/URN:NBN:no-82436
https://doi.org/10.1029/2019JC015906
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spelling ftoslouniv:oai:www.duo.uio.no:10852/79319 2023-05-15T17:43:27+02:00 Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation Strand, Kjersti Opstad Breivik, Øyvind Pedersen, Geir Vikebø, Frode Bendiksen Sundby, Svein Christensen, Kai Håkon 2020-07-20T14:29:10Z http://hdl.handle.net/10852/79319 http://urn.nb.no/URN:NBN:no-82436 https://doi.org/10.1029/2019JC015906 EN eng SIVA/237906 NFR/244262 http://urn.nb.no/URN:NBN:no-82436 Strand, Kjersti Opstad Breivik, Øyvind Pedersen, Geir Vikebø, Frode Bendiksen Sundby, Svein Christensen, Kai Håkon . Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation. Journal of Geophysical Research (JGR): Space Physics. 2020, 125(2) http://hdl.handle.net/10852/79319 1819881 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Geophysical Research (JGR): Space Physics&rft.volume=125&rft.spage=&rft.date=2020 Journal of Geophysical Research (JGR): Space Physics 125 2 14 https://doi.org/10.1029/2019JC015906 URN:NBN:no-82436 Fulltext https://www.duo.uio.no/bitstream/handle/10852/79319/2/2019JC015906.pdf Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 2169-9380 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2020 ftoslouniv https://doi.org/10.1029/2019JC015906 2020-09-16T22:30:08Z Air bubble penetration depths are investigated with a bottom‐mounted echosounder at a seabed observatory in northern Norway. We compare a 1‐year time series of observed bubble depth against modeled and estimated turbulent kinetic energy flux from breaking waves as well as wind speed and sea state. We find that the hourly mean and maximum bubble depths are highly variable, reaching 18 and 38 m, respectively, and strongly correlated with wind and sea state. The bubble depth is shallowest during summer following the seasonal variations in wind speed and wave height. Summertime shallowing of the mixed layer depth is not limiting the penetration depth. A strong relationship between bubble depth and modeled turbulent kinetic energy flux from breaking waves is found, similar in strength to the relationship between bubble depth and wind speed. The wind sea is more strongly correlated with bubble depth than the total significant wave height, and the swell is only weakly correlated, suggesting that the wave model does a reasonable separation of swell and wind sea. Article in Journal/Newspaper Northern Norway Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Norway Journal of Geophysical Research: Oceans 125 2
institution Open Polar
collection Universitet i Oslo: Digitale utgivelser ved UiO (DUO)
op_collection_id ftoslouniv
language English
description Air bubble penetration depths are investigated with a bottom‐mounted echosounder at a seabed observatory in northern Norway. We compare a 1‐year time series of observed bubble depth against modeled and estimated turbulent kinetic energy flux from breaking waves as well as wind speed and sea state. We find that the hourly mean and maximum bubble depths are highly variable, reaching 18 and 38 m, respectively, and strongly correlated with wind and sea state. The bubble depth is shallowest during summer following the seasonal variations in wind speed and wave height. Summertime shallowing of the mixed layer depth is not limiting the penetration depth. A strong relationship between bubble depth and modeled turbulent kinetic energy flux from breaking waves is found, similar in strength to the relationship between bubble depth and wind speed. The wind sea is more strongly correlated with bubble depth than the total significant wave height, and the swell is only weakly correlated, suggesting that the wave model does a reasonable separation of swell and wind sea.
format Article in Journal/Newspaper
author Strand, Kjersti Opstad
Breivik, Øyvind
Pedersen, Geir
Vikebø, Frode Bendiksen
Sundby, Svein
Christensen, Kai Håkon
spellingShingle Strand, Kjersti Opstad
Breivik, Øyvind
Pedersen, Geir
Vikebø, Frode Bendiksen
Sundby, Svein
Christensen, Kai Håkon
Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation
author_facet Strand, Kjersti Opstad
Breivik, Øyvind
Pedersen, Geir
Vikebø, Frode Bendiksen
Sundby, Svein
Christensen, Kai Håkon
author_sort Strand, Kjersti Opstad
title Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation
title_short Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation
title_full Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation
title_fullStr Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation
title_full_unstemmed Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation
title_sort long-term statistics of observed bubble depth versus modeled wave dissipation
publishDate 2020
url http://hdl.handle.net/10852/79319
http://urn.nb.no/URN:NBN:no-82436
https://doi.org/10.1029/2019JC015906
geographic Norway
geographic_facet Norway
genre Northern Norway
genre_facet Northern Norway
op_source 2169-9380
op_relation SIVA/237906
NFR/244262
http://urn.nb.no/URN:NBN:no-82436
Strand, Kjersti Opstad Breivik, Øyvind Pedersen, Geir Vikebø, Frode Bendiksen Sundby, Svein Christensen, Kai Håkon . Long-Term Statistics of Observed Bubble Depth Versus Modeled Wave Dissipation. Journal of Geophysical Research (JGR): Space Physics. 2020, 125(2)
http://hdl.handle.net/10852/79319
1819881
info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Geophysical Research (JGR): Space Physics&rft.volume=125&rft.spage=&rft.date=2020
Journal of Geophysical Research (JGR): Space Physics
125
2
14
https://doi.org/10.1029/2019JC015906
URN:NBN:no-82436
Fulltext https://www.duo.uio.no/bitstream/handle/10852/79319/2/2019JC015906.pdf
op_rights Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1029/2019JC015906
container_title Journal of Geophysical Research: Oceans
container_volume 125
container_issue 2
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