Modelling swell propagation across the Pacific

Ocean wave swell generated in the vicinity of Campbell Island in the Southern Ocean is tracked along Great Circle paths across the Pacific Ocean. Data from a wave buoy at Campbell Island provides data on the directional spectrum in the generation region. The swell is measured at locations along a se...

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Bibliographic Details
Published in:Frontiers in Marine Science
Main Authors: Sachini Pathirana, Ian Young, Alberto Meucci
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2023
Subjects:
Q
Online Access:https://doi.org/10.3389/fmars.2023.1187473
https://doaj.org/article/1ecceb06ebdd489db5d52da1ce18d6d5
id ftdoajarticles:oai:doaj.org/article:1ecceb06ebdd489db5d52da1ce18d6d5
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spelling ftdoajarticles:oai:doaj.org/article:1ecceb06ebdd489db5d52da1ce18d6d5 2023-08-20T04:09:57+02:00 Modelling swell propagation across the Pacific Sachini Pathirana Ian Young Alberto Meucci 2023-07-01T00:00:00Z https://doi.org/10.3389/fmars.2023.1187473 https://doaj.org/article/1ecceb06ebdd489db5d52da1ce18d6d5 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2023.1187473/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2023.1187473 https://doaj.org/article/1ecceb06ebdd489db5d52da1ce18d6d5 Frontiers in Marine Science, Vol 10 (2023) Ocean swell WAVEWATCH III wave modelling swell dissipation sentinel-1 SAR negative wind input Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2023 ftdoajarticles https://doi.org/10.3389/fmars.2023.1187473 2023-07-30T00:39:22Z Ocean wave swell generated in the vicinity of Campbell Island in the Southern Ocean is tracked along Great Circle paths across the Pacific Ocean. Data from a wave buoy at Campbell Island provides data on the directional spectrum in the generation region. The swell is measured at locations along a series of 19 Great Circle paths across the Pacific using Sentinel-1 SAR and CFOSAT satellite data. The WAVEWATCH III spectral wave model is used as a diagnostic tool to investigate the physical processes active in the swell propagation and decay. The results indicate that present day spectral wave models over-estimate the decay rate of swell. Although these models contain source terms to represent swell decay and negative wind input, these terms still largely remain tuning parameters. The data indicates that further research is required to adequately represent the observed magnitudes of the swell decay. In addition, the data show that currents have only a small impact on the observed swell decay and that islands can have a major impact. Such island impacts are poorly represented by spectral wave models. Article in Journal/Newspaper Southern Ocean Directory of Open Access Journals: DOAJ Articles Campbell Island ENVELOPE(169.500,169.500,-52.500,-52.500) Pacific Southern Ocean Frontiers in Marine Science 10
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ocean swell
WAVEWATCH III
wave modelling
swell dissipation
sentinel-1 SAR
negative wind input
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
spellingShingle Ocean swell
WAVEWATCH III
wave modelling
swell dissipation
sentinel-1 SAR
negative wind input
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
Sachini Pathirana
Ian Young
Alberto Meucci
Modelling swell propagation across the Pacific
topic_facet Ocean swell
WAVEWATCH III
wave modelling
swell dissipation
sentinel-1 SAR
negative wind input
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
description Ocean wave swell generated in the vicinity of Campbell Island in the Southern Ocean is tracked along Great Circle paths across the Pacific Ocean. Data from a wave buoy at Campbell Island provides data on the directional spectrum in the generation region. The swell is measured at locations along a series of 19 Great Circle paths across the Pacific using Sentinel-1 SAR and CFOSAT satellite data. The WAVEWATCH III spectral wave model is used as a diagnostic tool to investigate the physical processes active in the swell propagation and decay. The results indicate that present day spectral wave models over-estimate the decay rate of swell. Although these models contain source terms to represent swell decay and negative wind input, these terms still largely remain tuning parameters. The data indicates that further research is required to adequately represent the observed magnitudes of the swell decay. In addition, the data show that currents have only a small impact on the observed swell decay and that islands can have a major impact. Such island impacts are poorly represented by spectral wave models.
format Article in Journal/Newspaper
author Sachini Pathirana
Ian Young
Alberto Meucci
author_facet Sachini Pathirana
Ian Young
Alberto Meucci
author_sort Sachini Pathirana
title Modelling swell propagation across the Pacific
title_short Modelling swell propagation across the Pacific
title_full Modelling swell propagation across the Pacific
title_fullStr Modelling swell propagation across the Pacific
title_full_unstemmed Modelling swell propagation across the Pacific
title_sort modelling swell propagation across the pacific
publisher Frontiers Media S.A.
publishDate 2023
url https://doi.org/10.3389/fmars.2023.1187473
https://doaj.org/article/1ecceb06ebdd489db5d52da1ce18d6d5
long_lat ENVELOPE(169.500,169.500,-52.500,-52.500)
geographic Campbell Island
Pacific
Southern Ocean
geographic_facet Campbell Island
Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source Frontiers in Marine Science, Vol 10 (2023)
op_relation https://www.frontiersin.org/articles/10.3389/fmars.2023.1187473/full
https://doaj.org/toc/2296-7745
2296-7745
doi:10.3389/fmars.2023.1187473
https://doaj.org/article/1ecceb06ebdd489db5d52da1ce18d6d5
op_doi https://doi.org/10.3389/fmars.2023.1187473
container_title Frontiers in Marine Science
container_volume 10
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