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...

Full description

Bibliographic Details
Published in:Frontiers in Marine Science
Main Authors: Pathirana, Sachini, Young, Ian, Meucci, Alberto
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2023
Subjects:
Online Access:http://dx.doi.org/10.3389/fmars.2023.1187473
https://www.frontiersin.org/articles/10.3389/fmars.2023.1187473/full
id crfrontiers:10.3389/fmars.2023.1187473
record_format openpolar
spelling crfrontiers:10.3389/fmars.2023.1187473 2024-02-11T10:08:51+01:00 Modelling swell propagation across the Pacific Pathirana, Sachini Young, Ian Meucci, Alberto 2023 http://dx.doi.org/10.3389/fmars.2023.1187473 https://www.frontiersin.org/articles/10.3389/fmars.2023.1187473/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Marine Science volume 10 ISSN 2296-7745 Ocean Engineering Water Science and Technology Aquatic Science Global and Planetary Change Oceanography journal-article 2023 crfrontiers https://doi.org/10.3389/fmars.2023.1187473 2024-01-26T10:07:23Z 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 Frontiers (Publisher) Campbell Island ENVELOPE(169.500,169.500,-52.500,-52.500) Pacific Southern Ocean Frontiers in Marine Science 10
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
topic Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
spellingShingle Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
Pathirana, Sachini
Young, Ian
Meucci, Alberto
Modelling swell propagation across the Pacific
topic_facet Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
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 Pathirana, Sachini
Young, Ian
Meucci, Alberto
author_facet Pathirana, Sachini
Young, Ian
Meucci, Alberto
author_sort Pathirana, Sachini
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 SA
publishDate 2023
url http://dx.doi.org/10.3389/fmars.2023.1187473
https://www.frontiersin.org/articles/10.3389/fmars.2023.1187473/full
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
volume 10
ISSN 2296-7745
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fmars.2023.1187473
container_title Frontiers in Marine Science
container_volume 10
_version_ 1790608474607976448