Articles | Volume 14, issue 1
https://doi.org/10.5194/tc-14-93-2020
https://doi.org/10.5194/tc-14-93-2020
Research article
 | 
16 Jan 2020
Research article |  | 16 Jan 2020

Feature-based comparison of sea ice deformation in lead-permitting sea ice simulations

Nils Hutter and Martin Losch

Data sets

Linear Kinematic Features (leads & pressure ridges) detected and tracked in sea-ice deformation simulated in an Arc- tic configuration of MITgcm using a 2-km horizontal grid spacing from 1997 to 2008 N. Hutter https://doi.org/10.1594/PANGAEA.909636

Linear Kinematic Features (leads & pressure ridges) detected and tracked in sea-ice deformation simulated in an Arctic configuration of MITgcm using a 2-km horizontal grid with an active 5-class ice thickness distribution spacing from 1997 to 2008 N. Hutter https://doi.org/10.1594/PANGAEA.909632

Linear Kinematic Features (leads & pressure ridges) detected and tracked in RADARSAT Geophysical Processor System (RGPS) sea-ice deformation data from 1997 to 2008 N. Hutter, L. Zampieri, and M. Losch https://doi.org/10.1594/PANGAEA.898114

Model code and software

lkf_tools: a code to detect and track Linear Kinematic Features (LKFs) in sea-ice deformation data (Version v1.0) N. Hutter https://doi.org/10.5281/zenodo.2560078

Download
Short summary
Sea ice is composed of a multitude of floes that constantly deform due to wind and ocean currents and thereby form leads and pressure ridges. These features are visible in the ice as stripes of open-ocean or high-piled ice. High-resolution sea ice models start to resolve these deformation features. In this paper we present two simulations that agree with satellite data according to a new evaluation metric that detects deformation features and compares their spatial and temporal characteristics.