Articles | Volume 11, issue 5
https://doi.org/10.5194/tc-11-2117-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-2117-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Wave–ice interactions in the neXtSIM sea-ice model
Timothy D. Williams
CORRESPONDING AUTHOR
Nansen Environmental and Remote Sensing Center, Thormøhlensgate 47, N5006, Bergen, Norway and the Bjerknes Center for Climate Research, Bergen, Norway
Pierre Rampal
Nansen Environmental and Remote Sensing Center, Thormøhlensgate 47, N5006, Bergen, Norway and the Bjerknes Center for Climate Research, Bergen, Norway
Sylvain Bouillon
Nansen Environmental and Remote Sensing Center, Thormøhlensgate 47, N5006, Bergen, Norway and the Bjerknes Center for Climate Research, Bergen, Norway
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39 citations as recorded by crossref.
- Drift of Pancake Ice Floes in the Winter Antarctic Marginal Ice Zone During Polar Cyclones A. Alberello et al. 10.1029/2019JC015418
- Investigation of Oblique Flexural Gravity Wave Scattering by Two Submerged Thin Vertical Porous Barriers with Different Porosities A. Chanda & S. Bora 10.1061/(ASCE)EM.1943-7889.0002071
- Modelling attenuation of irregular wave fields by artificial ice floes in the laboratory A. Toffoli et al. 10.1098/rsta.2021.0255
- A two layer model for wave dissipation in sea ice G. Sutherland et al. 10.1016/j.apor.2019.03.023
- A model study of convergent dynamics in the marginal ice zone J. Auclair et al. 10.1098/rsta.2021.0261
- Wave-induced stress and breaking of sea ice in a coupled hydrodynamic discrete-element wave–ice model A. Herman 10.5194/tc-11-2711-2017
- Calculation of the destruction of ice structures by the grid-characteristic method on structured grids A. Favorskaya & I. Petrov 10.1016/j.procs.2021.09.151
- Growth of wave height with retreating ice cover in the Arctic J. Li et al. 10.1016/j.coldregions.2019.102790
- A collection of wet beam models for wave–ice interaction S. Tavakoli & A. Babanin 10.5194/tc-17-939-2023
- Marginal Ice Zone Thickness and Extent due to Wave Radiation Stress P. Sutherland & D. Dumont 10.1175/JPO-D-17-0167.1
- Altimetric observation of wave attenuation through the Antarctic marginal ice zone using ICESat-2 J. Brouwer et al. 10.5194/tc-16-2325-2022
- OpenMetBuoy-v2021: An Easy-to-Build, Affordable, Customizable, Open-Source Instrument for Oceanographic Measurements of Drift and Waves in Sea Ice and the Open Ocean J. Rabault et al. 10.3390/geosciences12030110
- Waves and Swells in High Wind and Extreme Fetches, Measurements in the Southern Ocean A. Babanin et al. 10.3389/fmars.2019.00361
- Numerical simulation on the breakup of an ice sheet induced by regular incident waves K. He et al. 10.1016/j.apor.2021.103024
- Multi-scale satellite observations of Arctic sea ice: new insight into the life cycle of the floe size distribution B. Hwang & Y. Wang 10.1098/rsta.2021.0259
- Scattering of Flexural Gravity Waves by a Pair of Submerged Vertical Porous Barriers Located Above a Porous Sea-Bed A. Chanda & S. Nandan Bora 10.1115/1.4051475
- A dataset of direct observations of sea ice drift and waves in ice J. Rabault et al. 10.1038/s41597-023-02160-9
- Estimating the elastic modulus of landfast ice from wave observations J. Voermans et al. 10.1017/jog.2023.63
- Estimation of Antarctic sea ice thickness through observation of wave attenuation F. De Santi et al. 10.1016/j.ocemod.2024.102421
- Interactions between Irregular Wave Fields and Sea Ice: A Physical Model for Wave Attenuation and Ice Breakup in an Ice Tank G. Passerotti et al. 10.1175/JPO-D-21-0238.1
- Ocean Wave Interactions with Sea Ice: A Reappraisal V. Squire 10.1146/annurev-fluid-010719-060301
- A Two‐Part Model for Wave‐Sea Ice Interaction: Attenuation and Break‐Up J. Kousal et al. 10.1029/2022JC018571
- Modelling the Arctic wave-affected marginal ice zone: a comparison with ICESat-2 observations G. Boutin et al. 10.1098/rsta.2021.0262
- A New Brittle Rheology and Numerical Framework for Large‐Scale Sea‐Ice Models E. Ólason et al. 10.1029/2021MS002685
- Wave–sea-ice interactions in a brittle rheological framework G. Boutin et al. 10.5194/tc-15-431-2021
- Sizes and Shapes of Sea Ice Floes Broken by Waves–A Case Study From the East Antarctic Coast A. Herman et al. 10.3389/feart.2021.655977
- Spectral Modeling of Ice-Induced Wave Decay Q. Liu et al. 10.1175/JPO-D-19-0187.1
- Wave-triggered breakup in the marginal ice zone generates lognormal floe size distributions: a simulation study N. Mokus & F. Montiel 10.5194/tc-16-4447-2022
- Towards a coupled model to investigate wave–sea ice interactions in the Arctic marginal ice zone G. Boutin et al. 10.5194/tc-14-709-2020
- Wave-driven mesoscale currents in a marginal ice zone H. Dai et al. 10.1016/j.ocemod.2018.11.006
- Marginal ice zone dynamics: history, definitions and research perspectives D. Dumont 10.1098/rsta.2021.0253
- On the multi-fractal scaling properties of sea ice deformation P. Rampal et al. 10.5194/tc-13-2457-2019
- Wave propagation in the marginal ice zone: connections and feedback mechanisms within the air–ice–ocean system J. Thomson 10.1098/rsta.2021.0251
- On transitions in water wave propagation through consolidated to broken sea ice covers J. Pitt & L. Bennetts 10.1098/rspa.2023.0862
- Modelling wave-induced sea ice break-up in the marginal ice zone F. Montiel & V. Squire 10.1098/rspa.2017.0258
- Floe-size distributions in laboratory ice broken by waves A. Herman et al. 10.5194/tc-12-685-2018
- Sensitivity study of the wave-driven current in an Arctic frazil-pancake ice zone X. Zhang et al. 10.1007/s13131-020-1560-x
- A floe size dependent scattering model in two- and three-dimensions for wave attenuation by ice floes M. Meylan et al. 10.1016/j.ocemod.2021.101779
- Finite Element Simulation of Crack Propagation in Ice Floes I. Gribanov et al. 10.1016/j.prostr.2024.06.013
Latest update: 17 Nov 2024
Short summary
As the Arctic sea ice extent drops, more ship traffic seeks to take advantage of this, and a need for better wave and sea ice forecasts arises. One aspect of this is the location of the sea ice edge. The waves here can be quite large, but they die away as they travel into the ice. This causes momentum to be transferred from the waves to the ice, causing ice drift. However, our study found that the effect of the wind drag had more impact on the ice edge position than the waves.
As the Arctic sea ice extent drops, more ship traffic seeks to take advantage of this, and a...