Simulating ice–wave interactions in the Laurentian Great Lakes using a fully coupled hydrodynamic–ice–wave model.

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Title: Simulating ice–wave interactions in the Laurentian Great Lakes using a fully coupled hydrodynamic–ice–wave model.
Authors: Javaherian, M. Javad1,2 (AUTHOR) mjava@umich.edu, Cannon, David1,2 (AUTHOR) djcannon@umich.edu, Wang, Jia3 (AUTHOR), Fujisaki-Manome, Ayumi2,4 (AUTHOR), Bai, Peng1,3 (AUTHOR), Zuo, Lei1 (AUTHOR)
Source: Ocean Modelling. Jun2025, Vol. 195, pN.PAG-N.PAG. 1p.
Subjects: Ice floes, Sea ice, Beach erosion, Ocean waves, Wave energy, Storm surges
Abstract: Hydrodynamic modeling in cold climate regions necessitates more sophisticated approaches that accurately simulate ice–wave interactions. Traditional models often overlook the complex coupling mechanisms between ice and ocean waves, especially the two-way processes where ice attenuates wave energy and waves break ice floes. This oversight can also intensify modeling challenges in coastal areas, including large lakes, where ice–wave interactions influence storm surges, high waves, and coastal erosion. To address this gap, this paper introduces an enhanced modeling approach that integrates both ice-induced wave attenuation and wave-induced ice breakage. To implement these processes, the Finite-Volume Community Ocean Model (FVCOM) is coupled with an unstructured-grid wave model (SWAN) and the unstructured-grid version of the Los Alamos Sea Ice Model (UG-CICE) to form the FVCOM–SWAVE–UG-CICE framework. Using this fully coupled model, simulations were conducted for the Great Lakes. Results of the modeled ice concentration, ice thickness, and significant wave heights were reported and validated against observational data from the U.S. National Ice Center (NIC) and in-situ under-ice measurements. To further study the coupling effects, results of the proposed model were also compared with those from no coupling and one-way coupling (focusing only on ice-induced wave attenuation) models. Comparative analyses demonstrated significant improvements in the predicted ice concentration with the proposed fully coupled model. These findings reveal the importance of incorporating ice–wave interactions in accurately predicting ice cover dynamics in freshwater systems. • A fully coupled hydrodynamic model is introduced to simulate ice–wave interactions. • The coupling consists of ice-induced wave attenuation and wave-induced ice breakage. • Model is implemented in the FVCOM–SWAVE–UG-CICE framework for the Great Lakes. • Results are validated with NIC observational data and in-situ under-ice measurements. • Coupling effects are evaluated on ice concentration, ice thickness and wave heights. [ABSTRACT FROM AUTHOR]
Copyright of Ocean Modelling is the property of Elsevier B.V. and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Simulating ice–wave interactions in the Laurentian Great Lakes using a fully coupled hydrodynamic–ice–wave model.
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  Data: <searchLink fieldCode="AR" term="%22Javaherian%2C+M%2E+Javad%22">Javaherian, M. Javad</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<i> mjava@umich.edu</i><br /><searchLink fieldCode="AR" term="%22Cannon%2C+David%22">Cannon, David</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<i> djcannon@umich.edu</i><br /><searchLink fieldCode="AR" term="%22Wang%2C+Jia%22">Wang, Jia</searchLink><relatesTo>3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Fujisaki-Manome%2C+Ayumi%22">Fujisaki-Manome, Ayumi</searchLink><relatesTo>2,4</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Bai%2C+Peng%22">Bai, Peng</searchLink><relatesTo>1,3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Zuo%2C+Lei%22">Zuo, Lei</searchLink><relatesTo>1</relatesTo> (AUTHOR)
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  Data: <searchLink fieldCode="DE" term="%22Ice+floes%22">Ice floes</searchLink><br /><searchLink fieldCode="DE" term="%22Sea+ice%22">Sea ice</searchLink><br /><searchLink fieldCode="DE" term="%22Beach+erosion%22">Beach erosion</searchLink><br /><searchLink fieldCode="DE" term="%22Ocean+waves%22">Ocean waves</searchLink><br /><searchLink fieldCode="DE" term="%22Wave+energy%22">Wave energy</searchLink><br /><searchLink fieldCode="DE" term="%22Storm+surges%22">Storm surges</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: Hydrodynamic modeling in cold climate regions necessitates more sophisticated approaches that accurately simulate ice–wave interactions. Traditional models often overlook the complex coupling mechanisms between ice and ocean waves, especially the two-way processes where ice attenuates wave energy and waves break ice floes. This oversight can also intensify modeling challenges in coastal areas, including large lakes, where ice–wave interactions influence storm surges, high waves, and coastal erosion. To address this gap, this paper introduces an enhanced modeling approach that integrates both ice-induced wave attenuation and wave-induced ice breakage. To implement these processes, the Finite-Volume Community Ocean Model (FVCOM) is coupled with an unstructured-grid wave model (SWAN) and the unstructured-grid version of the Los Alamos Sea Ice Model (UG-CICE) to form the FVCOM–SWAVE–UG-CICE framework. Using this fully coupled model, simulations were conducted for the Great Lakes. Results of the modeled ice concentration, ice thickness, and significant wave heights were reported and validated against observational data from the U.S. National Ice Center (NIC) and in-situ under-ice measurements. To further study the coupling effects, results of the proposed model were also compared with those from no coupling and one-way coupling (focusing only on ice-induced wave attenuation) models. Comparative analyses demonstrated significant improvements in the predicted ice concentration with the proposed fully coupled model. These findings reveal the importance of incorporating ice–wave interactions in accurately predicting ice cover dynamics in freshwater systems. • A fully coupled hydrodynamic model is introduced to simulate ice–wave interactions. • The coupling consists of ice-induced wave attenuation and wave-induced ice breakage. • Model is implemented in the FVCOM–SWAVE–UG-CICE framework for the Great Lakes. • Results are validated with NIC observational data and in-situ under-ice measurements. • Coupling effects are evaluated on ice concentration, ice thickness and wave heights. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: <i>Copyright of Ocean Modelling is the property of Elsevier B.V. and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1016/j.ocemod.2025.102513
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 1
        StartPage: N.PAG
    Subjects:
      – SubjectFull: Ice floes
        Type: general
      – SubjectFull: Sea ice
        Type: general
      – SubjectFull: Beach erosion
        Type: general
      – SubjectFull: Ocean waves
        Type: general
      – SubjectFull: Wave energy
        Type: general
      – SubjectFull: Storm surges
        Type: general
    Titles:
      – TitleFull: Simulating ice–wave interactions in the Laurentian Great Lakes using a fully coupled hydrodynamic–ice–wave model.
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            NameFull: Javaherian, M. Javad
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            NameFull: Cannon, David
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            NameFull: Wang, Jia
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            – D: 01
              M: 06
              Text: Jun2025
              Type: published
              Y: 2025
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