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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Published in:Journal of Marine Science and Engineering
Main Author: Mark Orzech
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
Online Access:https://doi.org/10.3390/jmse11102017
https://doaj.org/article/a62f41185241480fb94cbe25353f6cef
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spelling 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
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