Articles | Volume 18, issue 10
https://doi.org/10.5194/tc-18-4687-2024
https://doi.org/10.5194/tc-18-4687-2024
Research article
 | 
15 Oct 2024
Research article |  | 15 Oct 2024

Assessing the representation of Arctic sea ice and the marginal ice zone in ocean–sea ice reanalyses

Francesco Cocetta, Lorenzo Zampieri, Julia Selivanova, and Doroteaciro Iovino

Data sets

NOAA/NSIDC Climate Data Record of Passive Microwave Sea Ice Concentration W. Meier et al. https://doi.org/10.7265/EFMZ-2T65

Global Sea Ice Concentration Interim Climate Data Record Release 3 - DMSP OSI SAF https://doi.org/10.15770/EUM_SAF_OSI_0013

Global Ocean Ensemble Physics Reanalysis E.U. Copernicus Marine Service Information (CMEMS) https://doi.org/10.48670/moi-00024

Arctic Ocean Physics Reanalysis E.U. Copernicus Marine Service Information (CMEMS) https://doi.org/10.48670/moi-00007

Global Ocean OSTIA Sea Surface Temperature and Sea Ice Analysis E.U. Copernicus Marine Service Information (CMEMS) https://doi.org/10.48670/moi-00165

Model code and software

Scripts for "GREP reanalysis captures the evolution of the Arctic Marginal Ice Zone across timescales" F. Cocetta https://doi.org/10.5281/zenodo.10651276

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Short summary
Arctic sea ice is thinning and retreating because of global warming. Thus, the region is transitioning to a new state featuring an expansion of the marginal ice zone, a region where mobile ice interacts with waves from the open ocean. By analyzing 30 years of sea ice reconstructions that combine numerical models and observations, this paper proves that an ensemble of global ocean and sea ice reanalyses is an adequate tool for investigating the changing Arctic sea ice cover.