Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion

A model-data inversion is applied to a very large observational dataset collected in the Southern Ocean north of the Ross Sea during late autumn to early winter, producing estimates of the frequency-dependent rate of dissipation by sea ice. The modeling platform is WAVEWATCH III(R) which accounts fo...

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Main Authors: Rogers, W. Erick, Meylan, Michael H., Kohout, Alison L.
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2020
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2006.04978
https://arxiv.org/abs/2006.04978
id ftdatacite:10.48550/arxiv.2006.04978
record_format openpolar
spelling ftdatacite:10.48550/arxiv.2006.04978 2023-05-15T18:07:33+02:00 Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion Rogers, W. Erick Meylan, Michael H. Kohout, Alison L. 2020 https://dx.doi.org/10.48550/arxiv.2006.04978 https://arxiv.org/abs/2006.04978 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences Article CreativeWork article Preprint 2020 ftdatacite https://doi.org/10.48550/arxiv.2006.04978 2022-03-10T15:28:04Z A model-data inversion is applied to a very large observational dataset collected in the Southern Ocean north of the Ross Sea during late autumn to early winter, producing estimates of the frequency-dependent rate of dissipation by sea ice. The modeling platform is WAVEWATCH III(R) which accounts for non-stationarity, advection, wave generation, and other relevant processes. The resulting 9477 dissipation profiles are co-located with other variables such as ice thickness to quantify correlations which might be exploited in later studies to improve predictions. Mean dissipation profiles from the inversion are fitted to simple binomials. Variability about the mean profile is not small, but the binomials show remarkable qualitative similarity to prior observation-based estimates of dissipation, and the power dependence is consistent with at least three theoretical models, one of which assumes that dissipation is dominated by turbulence generated by shear at the ice-water interface. : I am unfortunately not able to upload the Supplemental Information due to arxiv 10 MB limit on file size Article in Journal/Newspaper Ross Sea Sea ice Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Ross Sea Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
Rogers, W. Erick
Meylan, Michael H.
Kohout, Alison L.
Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
description A model-data inversion is applied to a very large observational dataset collected in the Southern Ocean north of the Ross Sea during late autumn to early winter, producing estimates of the frequency-dependent rate of dissipation by sea ice. The modeling platform is WAVEWATCH III(R) which accounts for non-stationarity, advection, wave generation, and other relevant processes. The resulting 9477 dissipation profiles are co-located with other variables such as ice thickness to quantify correlations which might be exploited in later studies to improve predictions. Mean dissipation profiles from the inversion are fitted to simple binomials. Variability about the mean profile is not small, but the binomials show remarkable qualitative similarity to prior observation-based estimates of dissipation, and the power dependence is consistent with at least three theoretical models, one of which assumes that dissipation is dominated by turbulence generated by shear at the ice-water interface. : I am unfortunately not able to upload the Supplemental Information due to arxiv 10 MB limit on file size
format Article in Journal/Newspaper
author Rogers, W. Erick
Meylan, Michael H.
Kohout, Alison L.
author_facet Rogers, W. Erick
Meylan, Michael H.
Kohout, Alison L.
author_sort Rogers, W. Erick
title Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion
title_short Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion
title_full Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion
title_fullStr Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion
title_full_unstemmed Estimates of dissipation of wave energy by sea ice for a field experiment in the Southern Ocean, using model/data inversion
title_sort estimates of dissipation of wave energy by sea ice for a field experiment in the southern ocean, using model/data inversion
publisher arXiv
publishDate 2020
url https://dx.doi.org/10.48550/arxiv.2006.04978
https://arxiv.org/abs/2006.04978
geographic Ross Sea
Southern Ocean
geographic_facet Ross Sea
Southern Ocean
genre Ross Sea
Sea ice
Southern Ocean
genre_facet Ross Sea
Sea ice
Southern Ocean
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.2006.04978
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