Scaling Properties of Arctic Sea Ice Deformation in a High‐Resolution Viscous‐Plastic Sea Ice Model and in Satellite Observations. Issue 1 (29th January 2018)

• Record Type: Journal Article
• Authors: Hutter, Nils; Losch, Martin; Menemenlis, Dimitris
• Is Part Of: Journal of geophysical research. Volume 123:Issue 1(2018)
• Page Start: 672
• Page End: 687
• Publication Date: 2018-01-29
• Subjects: sea ice deformation -- scaling -- Arctic Ocean -- sea ice rheology -- high‐resolution modeling; Oceanography -- Periodicals; 551.4605
• DOI: 10.1002/2017JC013119
• Languages: English
• ISSNs: 2169-9275

Abstract

Abstract: Sea ice models with the traditional viscous‐plastic (VP) rheology and very small horizontal grid spacing can resolve leads and deformation rates localized along Linear Kinematic Features (LKF). In a 1 km pan‐Arctic sea ice‐ocean simulation, the small‐scale sea ice deformations are evaluated with a scaling analysis in relation to satellite observations of the Envisat Geophysical Processor System (EGPS) in the Central Arctic. A new coupled scaling analysis for data on Eulerian grids is used to determine the spatial and temporal scaling and the coupling between temporal and spatial scales. The spatial scaling of the modeled sea ice deformation implies multifractality. It is also coupled to temporal scales and varies realistically by region and season. The agreement of the spatial scaling with satellite observations challenges previous results with VP models at coarser resolution, which did not reproduce the observed scaling. The temporal scaling analysis shows that the VP model, as configured in this 1 km simulation, does not fully resolve the intermittency of sea ice deformation that is observed in satellite data. Key Points: Sea ice deformation localizes along lines in high‐resolution viscous‐plastic sea ice models The model reproduces spatial scaling properties also observed in satellite data The model underestimates temporal scaling compared to satellite data