Articles | Volume 13, issue 11
https://doi.org/10.5194/tc-13-2869-2019
© Author(s) 2019. 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-13-2869-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Estimating the sea ice floe size distribution using satellite altimetry: theory, climatology, and model comparison
Institute at Brown for Environment and Society, Brown University, Providence, RI, USA
Lettie A. Roach
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
National Institute of Water and Atmospheric Research, Wellington, New Zealand
Rachel Tilling
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
Cecilia M. Bitz
Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
Baylor Fox-Kemper
Institute at Brown for Environment and Society, Brown University, Providence, RI, USA
Colin Guider
Department of Mathematics, University of North Carolina, Chapel Hill, NC, USA
Kaitlin Hill
School of Mathematics, University of Minnesota, Minneapolis, MN, USA
Andy Ridout
Centre for Polar Observation and Modelling, University College London, London, UK
Andrew Shepherd
Centre for Polar Observation and Modelling, University of Leeds, Leeds, UK
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- Wave–sea-ice interactions in a brittle rheological framework G. Boutin et al. 10.5194/tc-15-431-2021
- A dataset of direct observations of sea ice drift and waves in ice J. Rabault et al. 10.1038/s41597-023-02160-9
- Modelling the Arctic wave-affected marginal ice zone: a comparison with ICESat-2 observations G. Boutin et al. 10.1098/rsta.2021.0262
- A method for constructing directional surface wave spectra from ICESat-2 altimetry M. Hell & C. Horvat 10.5194/tc-18-341-2024
- 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
- Impact of sea ice floe size distribution on seasonal fragmentation and melt of Arctic sea ice A. Bateson et al. 10.5194/tc-14-403-2020
- Advances in Modeling Interactions Between Sea Ice and Ocean Surface Waves L. Roach et al. 10.1029/2019MS001836
- SubZero: A Sea Ice Model With an Explicit Representation of the Floe Life Cycle G. Manucharyan & B. Montemuro 10.1029/2022MS003247
- 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
- Contemporary and historical detection of small lakes using super resolution Landsat imagery: promise and peril E. Kyzivat & L. Smith 10.1080/15481603.2023.2207288
- Altimetric observation of wave attenuation through the Antarctic marginal ice zone using ICESat-2 J. Brouwer et al. 10.5194/tc-16-2325-2022
- 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
- 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
- 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 Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys J. Negrel et al. 10.1017/aog.2020.61
- 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
- Co-located OLCI optical imagery and SAR altimetry from Sentinel-3 for enhanced Arctic spring sea ice surface classification W. Chen et al. 10.3389/frsen.2024.1401653
- 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
- Parameterization of Submesoscale Mixed Layer Restratification under Sea Ice K. Shrestha & G. Manucharyan 10.1175/JPO-D-21-0024.1
- 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
- Observing Waves in Sea Ice With ICESat‐2 C. Horvat et al. 10.1029/2020GL087629
- Spinning ice floes reveal intensification of mesoscale eddies in the western Arctic Ocean G. Manucharyan et al. 10.1038/s41598-022-10712-z
- A High-Resolution Airborne Color-Infrared Camera Water Mask for the NASA ABoVE Campaign E. Kyzivat et al. 10.3390/rs11182163
22 citations as recorded by crossref.
- Wave–sea-ice interactions in a brittle rheological framework G. Boutin et al. 10.5194/tc-15-431-2021
- A dataset of direct observations of sea ice drift and waves in ice J. Rabault et al. 10.1038/s41597-023-02160-9
- Modelling the Arctic wave-affected marginal ice zone: a comparison with ICESat-2 observations G. Boutin et al. 10.1098/rsta.2021.0262
- A method for constructing directional surface wave spectra from ICESat-2 altimetry M. Hell & C. Horvat 10.5194/tc-18-341-2024
- 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
- Impact of sea ice floe size distribution on seasonal fragmentation and melt of Arctic sea ice A. Bateson et al. 10.5194/tc-14-403-2020
- Advances in Modeling Interactions Between Sea Ice and Ocean Surface Waves L. Roach et al. 10.1029/2019MS001836
- SubZero: A Sea Ice Model With an Explicit Representation of the Floe Life Cycle G. Manucharyan & B. Montemuro 10.1029/2022MS003247
- 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
- Contemporary and historical detection of small lakes using super resolution Landsat imagery: promise and peril E. Kyzivat & L. Smith 10.1080/15481603.2023.2207288
- Altimetric observation of wave attenuation through the Antarctic marginal ice zone using ICESat-2 J. Brouwer et al. 10.5194/tc-16-2325-2022
- 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
- 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
- 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 Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys J. Negrel et al. 10.1017/aog.2020.61
- 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
- Co-located OLCI optical imagery and SAR altimetry from Sentinel-3 for enhanced Arctic spring sea ice surface classification W. Chen et al. 10.3389/frsen.2024.1401653
- 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
- Parameterization of Submesoscale Mixed Layer Restratification under Sea Ice K. Shrestha & G. Manucharyan 10.1175/JPO-D-21-0024.1
- 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
- Observing Waves in Sea Ice With ICESat‐2 C. Horvat et al. 10.1029/2020GL087629
- Spinning ice floes reveal intensification of mesoscale eddies in the western Arctic Ocean G. Manucharyan et al. 10.1038/s41598-022-10712-z
1 citations as recorded by crossref.
Latest update: 14 Dec 2024
Short summary
Changes in the floe size distribution (FSD) are important for sea ice evolution but to date largely unobserved and unknown. Climate models, forecast centres, ship captains, and logistic specialists cannot currently obtain statistical information about sea ice floe size on demand. We develop a new method to observe the FSD at global scales and high temporal and spatial resolution. With refinement, this method can provide crucial information for polar ship routing and real-time forecasting.
Changes in the floe size distribution (FSD) are important for sea ice evolution but to date...