Articles | Volume 14, issue 6
https://doi.org/10.5194/tc-14-1971-2020
© 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-14-1971-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Changes of the Arctic marginal ice zone during the satellite era
Centre for Polar Observation and Modelling, Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
now at: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
Daniel L. Feltham
Centre for Polar Observation and Modelling, Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
David Schröder
Centre for Polar Observation and Modelling, Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
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32 citations as recorded by crossref.
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- Floes, the marginal ice zone and coupled wave-sea-ice feedbacks C. Horvat 10.1098/rsta.2021.0252
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- The Antarctic Marginal Ice Zone and Pack Ice Area in CMEMS GREP Ensemble Reanalysis Product D. Iovino et al. 10.3389/feart.2022.745274
- The role of boundary layer processes in summer-time Arctic cyclones H. Croad et al. 10.5194/wcd-4-617-2023
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- Data-driven surrogate modeling of high-resolution sea-ice thickness in the Arctic C. Durand et al. 10.5194/tc-18-1791-2024
- Influence of sea-ice-related features and anthropogenic subsidies on the foraging behaviour of a high-Arctic seabird, the ivory gull (Pagophila eburnea) K. Dumas et al. 10.1007/s00227-022-04137-5
- Marginal ice zone dynamics: history, definitions and research perspectives D. Dumont 10.1098/rsta.2021.0253
- Scale‐Dependent Air‐Sea Exchange in the Polar Oceans: Floe‐Floe and Floe‐Flow Coupling in the Generation of Ice‐Ocean Boundary Layer Turbulence S. Brenner et al. 10.1029/2023GL105703
- Ship-based estimates of momentum transfer coefficient over sea ice and recommendations for its parameterization P. Srivastava et al. 10.5194/acp-22-4763-2022
- PREDICTION OF THE ANTARCTIC MARGINAL ICE ZONE EXTENT BASED UPON ITS MULTIFRACTAL PROPERTY Y. LIU et al. 10.1142/S0218348X21500353
- An indicator of sea ice variability for the Antarctic marginal ice zone M. Vichi 10.5194/tc-16-4087-2022
- Atmospheric drivers of a winter-to-spring Lagrangian sea-ice drift in the Eastern Antarctic marginal ice zone A. Womack et al. 10.1017/jog.2022.14
- Wave Attenuation by Sea Ice in the Arctic Marginal Ice Zone Observed by Spaceborne SAR B. Huang & X. Li 10.1029/2023GL105059
- Airborne measurements of directional reflectivity over the Arctic marginal sea ice zone S. Becker et al. 10.5194/amt-15-2939-2022
- Modelling the Arctic wave-affected marginal ice zone: a comparison with ICESat-2 observations G. Boutin et al. 10.1098/rsta.2021.0262
- Multiscale mushy layer model for Arctic marginal ice zone dynamics C. Strong et al. 10.1038/s41598-024-70868-8
- Mechanisms and Impacts of Earth System Tipping Elements S. Wang et al. 10.1029/2021RG000757
- 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
- Eddy‐Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone M. Gupta et al. 10.1029/2023GL105656
- On the definition of the marginal ice zone: a case study with SAR and passive microwave data A. Soleymani et al. 10.1088/2515-7620/ad82b4
- 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
- Past and future of the Arctic sea ice in High-Resolution Model Intercomparison Project (HighResMIP) climate models J. Selivanova et al. 10.5194/tc-18-2739-2024
Latest update: 13 Dec 2024
Short summary
It is well known that the Arctic sea ice extent is declining, and it is often assumed that the marginal ice zone (MIZ), the area of partial sea ice cover, is consequently increasing. However, we find no trend in the MIZ extent during the last 40 years from observations that is consistent with a widening of the MIZ as it moves northward. Differences of MIZ extent between different satellite retrievals are too large to provide a robust basis to verify model simulations of MIZ extent.
It is well known that the Arctic sea ice extent is declining, and it is often assumed that the...