Articles | Volume 14, issue 2
https://doi.org/10.5194/tc-14-403-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-403-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Impact of sea ice floe size distribution on seasonal fragmentation and melt of Arctic sea ice
Adam W. Bateson
CORRESPONDING AUTHOR
Department of Meteorology, University of Reading, Reading, RG2 7PS,
UK
Daniel L. Feltham
Department of Meteorology, University of Reading, Reading, RG2 7PS,
UK
David Schröder
Department of Meteorology, University of Reading, Reading, RG2 7PS,
UK
Lucia Hosekova
Department of Meteorology, University of Reading, Reading, RG2 7PS,
UK
Jeff K. Ridley
Hadley Centre for Climate Prediction and Research, Met Office, Exeter, EX1 3PB, UK
Yevgeny Aksenov
National Oceanography Centre Southampton, Southampton, SO14 3ZH, UK
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43 citations as recorded by crossref.
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- Theoretical model for predicting the break-up of ice covers due to wave-ice interaction C. Zhang & X. Zhao 10.1016/j.apor.2021.102614
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- A Two‐Part Model for Wave‐Sea Ice Interaction: Attenuation and Break‐Up J. Kousal et al. 10.1029/2022JC018571
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- Projected changes in sea ice and the navigability of the Arctic Passages under global warming of 2 ℃ and 3 ℃ J. Chen et al. 10.1016/j.ancene.2022.100349
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- Advances in Modeling Interactions Between Sea Ice and Ocean Surface Waves L. Roach et al. 10.1029/2019MS001836
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39 citations as recorded by crossref.
- Sea ice floe size: its impact on pan-Arctic and local ice mass and required model complexity A. Bateson et al. 10.5194/tc-16-2565-2022
- Effects of Wave-Induced Sea Ice Break-Up and Mixing in a High-Resolution Coupled Ice-Ocean Model J. Li et al. 10.3390/jmse9040365
- Theoretical framework for the emergent floe size distribution in the marginal ice zone: the case for log-normality F. Montiel & N. Mokus 10.1098/rsta.2021.0257
- Theoretical model for predicting the break-up of ice covers due to wave-ice interaction C. Zhang & X. Zhao 10.1016/j.apor.2021.102614
- Priority Organic Pollutants and Endocrine‐Disrupting Compounds in Arctic Marine Sediments (Svalbard Islands, Norway) F. Spataro et al. 10.1002/etc.5334
- Wind-wave climate changes and their impacts M. Casas-Prat et al. 10.1038/s43017-023-00502-0
- On transitions in water wave propagation through consolidated to broken sea ice covers J. Pitt & L. Bennetts 10.1098/rspa.2023.0862
- Arctic sea ice sensitivity to lateral melting representation in a coupled climate model M. Smith et al. 10.5194/tc-16-419-2022
- Impact of horizontal resolution on global ocean–sea ice model simulations based on the experimental protocols of the Ocean Model Intercomparison Project phase 2 (OMIP-2) E. Chassignet et al. 10.5194/gmd-13-4595-2020
- 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
- A Two‐Part Model for Wave‐Sea Ice Interaction: Attenuation and Break‐Up J. Kousal et al. 10.1029/2022JC018571
- An improved regional coupled modeling system for Arctic sea ice simulation and prediction: a case study for 2018 C. Yang et al. 10.5194/gmd-15-1155-2022
- Summer sea ice floe perimeter density in the Arctic: high-resolution optical satellite imagery and model evaluation Y. Wang et al. 10.5194/tc-17-3575-2023
- Marginal ice zone fraction benchmarks sea ice and climate model skill C. Horvat 10.1038/s41467-021-22004-7
- 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
- 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
- The seasonal cycle and break-up of landfast sea ice along the northwest coast of Kotelny Island, East Siberian Sea M. Zhai et al. 10.1017/jog.2021.85
- 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
- Glucose Enhances Salinity-Driven Sea Spray Aerosol Production in Eastern Arctic Waters A. Rocchi et al. 10.1021/acs.est.4c02826
- Floes, the marginal ice zone and coupled wave-sea-ice feedbacks C. Horvat 10.1098/rsta.2021.0252
- Characterizing the sea-ice floe size distribution in the Canada Basin from high-resolution optical satellite imagery A. Denton & M. Timmermans 10.5194/tc-16-1563-2022
- Laboratory Studies on the Parametrization Scheme of the Melting Rate of Ice–Air and Ice–Water Interfaces Z. Li et al. 10.3390/w14111775
- Regimes of Sea‐Ice Floe Melt: Ice‐Ocean Coupling at the Submesoscales M. Gupta & A. Thompson 10.1029/2022JC018894
- Applying landscape fragmentation analysis to icescape environments: potential impacts for the Pacific walrus (Odobenus rosmarus divergens) A. Himmelberger et al. 10.33265/polar.v41.5169
- Understanding the influence of ocean waves on Arctic sea ice simulation: a modeling study with an atmosphere–ocean–wave–sea ice coupled model C. Yang et al. 10.5194/tc-18-1215-2024
- WIFF1.0: a hybrid machine-learning-based parameterization of wave-induced sea ice floe fracture C. Horvat & L. Roach 10.5194/gmd-15-803-2022
- Impacts of 1.5 °C global warming on hydrological conditions of navigation along the Northern Sea Route and Northwest Passage J. Chen et al. 10.1016/j.accre.2023.11.010
- A STUDY OF SEA ICE FLOE DISTRIBUTION ON OKHOTSK SEA COAST OF HOKKAIDO S. KIOKA et al. 10.2208/jscejoe.76.2_I_905
- Climate change hotspots and implications for the global subsea telecommunications network M. Clare et al. 10.1016/j.earscirev.2022.104296
- Changes of the Arctic marginal ice zone during the satellite era R. Rolph et al. 10.5194/tc-14-1971-2020
- Granular effects in sea ice rheology in the marginal ice zone A. Herman 10.1098/rsta.2021.0260
- Aerial observations of sea ice breakup by ship waves E. Dumas-Lefebvre & D. Dumont 10.5194/tc-17-827-2023
- Observing Waves in Sea Ice With ICESat‐2 C. Horvat et al. 10.1029/2020GL087629
- Scattering kernel of an array of floating ice floes: application to water wave transport in the marginal ice zone F. Montiel et al. 10.1098/rspa.2023.0633
- Wind waves in sea ice of the western Arctic and a global coupled wave-ice model V. Cooper et al. 10.1098/rsta.2021.0258
- Wave–sea-ice interactions in a brittle rheological framework G. Boutin et al. 10.5194/tc-15-431-2021
- Modelling the Arctic wave-affected marginal ice zone: a comparison with ICESat-2 observations G. Boutin et al. 10.1098/rsta.2021.0262
- DynIceData: a gridded ice–water classification dataset at short-time intervals based on observations from multiple satellites over the marginal ice zone L. Huang et al. 10.1080/20964471.2023.2230714
- Projected changes in sea ice and the navigability of the Arctic Passages under global warming of 2 ℃ and 3 ℃ J. Chen et al. 10.1016/j.ancene.2022.100349
4 citations as recorded by crossref.
- Estimating the sea ice floe size distribution using satellite altimetry: theory, climatology, and model comparison C. Horvat et al. 10.5194/tc-13-2869-2019
- 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
- Advances in Modeling Interactions Between Sea Ice and Ocean Surface Waves L. Roach et al. 10.1029/2019MS001836
- Wave energy attenuation in fields of colliding ice floes – Part 1: Discrete-element modelling of dissipation due to ice–water drag A. Herman et al. 10.5194/tc-13-2887-2019
Latest update: 20 Nov 2024
Short summary
The Arctic sea ice cover has been observed to be decreasing, particularly in summer. We use numerical models to gain insight into processes controlling its seasonal and decadal evolution. Sea ice is made of pieces of ice called floes. Previous models have set these floes to be the same size, which is not supported by observations. In this study we show that accounting for variable floe size reveals the importance of sea ice regions close to the open ocean in driving seasonal retreat of sea ice.
The Arctic sea ice cover has been observed to be decreasing, particularly in summer. We use...