A New Method for Modeling Effects of Surface Ice on Waves
Accurate prediction of ocean surface wave attenuation in polar marginal ice zones remains a challenge. In this article, an alternative approach to the problem is introduced, in which the ice layer is represented with a modified version of the vegetation damping parameterization in a phase-resolved w...
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2023
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ftdoajarticles:oai:doaj.org/article:a62f41185241480fb94cbe25353f6cef 2023-11-12T04:26:01+01:00 A New Method for Modeling Effects of Surface Ice on Waves Mark Orzech 2023-10-01T00:00:00Z https://doi.org/10.3390/jmse11102017 https://doaj.org/article/a62f41185241480fb94cbe25353f6cef EN eng MDPI AG https://www.mdpi.com/2077-1312/11/10/2017 https://doaj.org/toc/2077-1312 doi:10.3390/jmse11102017 2077-1312 https://doaj.org/article/a62f41185241480fb94cbe25353f6cef Journal of Marine Science and Engineering, Vol 11, Iss 2017, p 2017 (2023) ocean surface waves sea ice marginal ice zone wave attenuation wave modeling Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 article 2023 ftdoajarticles https://doi.org/10.3390/jmse11102017 2023-10-29T00:36:17Z Accurate prediction of ocean surface wave attenuation in polar marginal ice zones remains a challenge. In this article, an alternative approach to the problem is introduced, in which the ice layer is represented with a modified version of the vegetation damping parameterization in a phase-resolved wave model. The new representation is evaluated by comparison to theory and measured data under varied wave and ice conditions. Model-estimated profiles of RMS water velocity and Reynolds stress under ice layers with different drag coefficients are found to be qualitatively comparable to a range of nondimensional profiles computed using viscous layer theory. Modeled profiles appear somewhat vertically “stretched” relative to theoretical results, and in this respect, they more closely resemble measurements obtained during a recent wave–ice laboratory experiment. Estimated values of the wave attenuation coefficient and wavenumber in ice from the adapted model align well with theory and with a range of lab and field datasets. Several additional model ice parameters are available to facilitate a more nuanced representation of surface ice effects and will be investigated further in an upcoming companion study. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles Journal of Marine Science and Engineering 11 10 2017 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
ocean surface waves sea ice marginal ice zone wave attenuation wave modeling Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 |
spellingShingle |
ocean surface waves sea ice marginal ice zone wave attenuation wave modeling Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 Mark Orzech A New Method for Modeling Effects of Surface Ice on Waves |
topic_facet |
ocean surface waves sea ice marginal ice zone wave attenuation wave modeling Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 |
description |
Accurate prediction of ocean surface wave attenuation in polar marginal ice zones remains a challenge. In this article, an alternative approach to the problem is introduced, in which the ice layer is represented with a modified version of the vegetation damping parameterization in a phase-resolved wave model. The new representation is evaluated by comparison to theory and measured data under varied wave and ice conditions. Model-estimated profiles of RMS water velocity and Reynolds stress under ice layers with different drag coefficients are found to be qualitatively comparable to a range of nondimensional profiles computed using viscous layer theory. Modeled profiles appear somewhat vertically “stretched” relative to theoretical results, and in this respect, they more closely resemble measurements obtained during a recent wave–ice laboratory experiment. Estimated values of the wave attenuation coefficient and wavenumber in ice from the adapted model align well with theory and with a range of lab and field datasets. Several additional model ice parameters are available to facilitate a more nuanced representation of surface ice effects and will be investigated further in an upcoming companion study. |
format |
Article in Journal/Newspaper |
author |
Mark Orzech |
author_facet |
Mark Orzech |
author_sort |
Mark Orzech |
title |
A New Method for Modeling Effects of Surface Ice on Waves |
title_short |
A New Method for Modeling Effects of Surface Ice on Waves |
title_full |
A New Method for Modeling Effects of Surface Ice on Waves |
title_fullStr |
A New Method for Modeling Effects of Surface Ice on Waves |
title_full_unstemmed |
A New Method for Modeling Effects of Surface Ice on Waves |
title_sort |
new method for modeling effects of surface ice on waves |
publisher |
MDPI AG |
publishDate |
2023 |
url |
https://doi.org/10.3390/jmse11102017 https://doaj.org/article/a62f41185241480fb94cbe25353f6cef |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Journal of Marine Science and Engineering, Vol 11, Iss 2017, p 2017 (2023) |
op_relation |
https://www.mdpi.com/2077-1312/11/10/2017 https://doaj.org/toc/2077-1312 doi:10.3390/jmse11102017 2077-1312 https://doaj.org/article/a62f41185241480fb94cbe25353f6cef |
op_doi |
https://doi.org/10.3390/jmse11102017 |
container_title |
Journal of Marine Science and Engineering |
container_volume |
11 |
container_issue |
10 |
container_start_page |
2017 |
_version_ |
1782340165364088832 |