Articles | Volume 16, issue 2
https://doi.org/10.5194/tc-16-419-2022
© Author(s) 2022. 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-16-419-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Feb 2022
Research article |
| 04 Feb 2022
| 04 Feb 2022
Arctic sea ice sensitivity to lateral melting representation in a coupled climate model
Applied Physics Laboratory, University of Washington, Seattle, Washington, USA
Marika Holland
National Center for Atmospheric Research, Boulder, Colorado, USA
Bonnie Light
Applied Physics Laboratory, University of Washington, Seattle, Washington, USA
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Cited
16 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
- Laboratory Studies on the Parametrization Scheme of the Melting Rate of Ice–Air and Ice–Water Interfaces Z. Li et al. 10.3390/w14111775
- Simple Hybrid Sea Ice Nudging Method for Improving Control Over Partitioning of Sea Ice Concentration and Thickness A. Audette & P. Kushner 10.1029/2022MS003180
- Arctic sea ice sensitivity to lateral melting representation in a coupled climate model M. Smith et al. 10.5194/tc-16-419-2022
- Physics of the Seasonal Sea Ice Zone L. Roach et al. 10.1146/annurev-marine-121422-015323
- 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
- Sensitivity of the Arctic Sea Ice Cover to the Summer Surface Scattering Layer M. Smith et al. 10.1029/2022GL098349
- Floes, the marginal ice zone and coupled wave-sea-ice feedbacks C. Horvat 10.1098/rsta.2021.0252
- Formation and fate of freshwater on an ice floe in the Central Arctic M. Smith et al. 10.5194/tc-19-619-2025
- Thin and transient meltwater layers and false bottoms in the Arctic sea ice pack—Recent insights on these historically overlooked features M. Smith et al. 10.1525/elementa.2023.00025
- Deep Learning of Systematic Sea Ice Model Errors From Data Assimilation Increments W. Gregory et al. 10.1029/2023MS003757
- Level Set Discrete Element Method for modeling sea ice floes R. Moncada et al. 10.1016/j.cma.2023.115891
- Influence of seasonally varying sea-ice concentration and subsurface ocean heat on sea-ice thickness and sea-ice seasonality for a ‘warm-shelf’ region in Antarctica B. Saenz et al. 10.1017/jog.2023.36
- 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
- Effects of Increasing the Category Resolution of the Sea Ice Thickness Distribution in a Coupled Climate Model on Arctic and Antarctic Sea Ice Mean State M. Smith et al. 10.1029/2022JC019044
- Impact of Ocean Heat Transport on Arctic Sea Ice Variability in the GFDL CM2‐O Model Suite M. Decuypère et al. 10.1029/2021JC017762
15 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
- Laboratory Studies on the Parametrization Scheme of the Melting Rate of Ice–Air and Ice–Water Interfaces Z. Li et al. 10.3390/w14111775
- Simple Hybrid Sea Ice Nudging Method for Improving Control Over Partitioning of Sea Ice Concentration and Thickness A. Audette & P. Kushner 10.1029/2022MS003180
- Arctic sea ice sensitivity to lateral melting representation in a coupled climate model M. Smith et al. 10.5194/tc-16-419-2022
- Physics of the Seasonal Sea Ice Zone L. Roach et al. 10.1146/annurev-marine-121422-015323
- 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
- Sensitivity of the Arctic Sea Ice Cover to the Summer Surface Scattering Layer M. Smith et al. 10.1029/2022GL098349
- Floes, the marginal ice zone and coupled wave-sea-ice feedbacks C. Horvat 10.1098/rsta.2021.0252
- Formation and fate of freshwater on an ice floe in the Central Arctic M. Smith et al. 10.5194/tc-19-619-2025
- Thin and transient meltwater layers and false bottoms in the Arctic sea ice pack—Recent insights on these historically overlooked features M. Smith et al. 10.1525/elementa.2023.00025
- Deep Learning of Systematic Sea Ice Model Errors From Data Assimilation Increments W. Gregory et al. 10.1029/2023MS003757
- Level Set Discrete Element Method for modeling sea ice floes R. Moncada et al. 10.1016/j.cma.2023.115891
- Influence of seasonally varying sea-ice concentration and subsurface ocean heat on sea-ice thickness and sea-ice seasonality for a ‘warm-shelf’ region in Antarctica B. Saenz et al. 10.1017/jog.2023.36
- 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
- Effects of Increasing the Category Resolution of the Sea Ice Thickness Distribution in a Coupled Climate Model on Arctic and Antarctic Sea Ice Mean State M. Smith et al. 10.1029/2022JC019044
1 citations as recorded by crossref.
Latest update: 19 May 2025
Short summary
Climate models represent the atmosphere, ocean, sea ice, and land with equations of varying complexity and are important tools for understanding changes in global climate. Here, we explore how realistic variations in the equations describing how sea ice melt occurs at the edges (called lateral melting) impact ice and climate. We find that these changes impact the progression of the sea-ice–albedo feedback in the Arctic and so make significant changes to the predicted Arctic sea ice.
Climate models represent the atmosphere, ocean, sea ice, and land with equations of varying...
