Deformation lines in Arctic sea ice: intersection angles distribution and mechanical properties - codes and intersection angle data

Code and data to reproduce the results presented in Ringeisen et al. (2023). The included notebooks compute intersection angle distributions and distributions of deformation rates along LKFs, as well as derive yield curves from intersection angle distributions. The intersection angle data sets have...

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Bibliographic Details
Main Authors: Nils Hutter, Damien Ringeisen, Luisa von Albedyl
Format: Software
Language:unknown
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/8125554
https://doi.org/10.5281/zenodo.8125554
Description
Summary:Code and data to reproduce the results presented in Ringeisen et al. (2023). The included notebooks compute intersection angle distributions and distributions of deformation rates along LKFs, as well as derive yield curves from intersection angle distributions. The intersection angle data sets have been extracted from three different LKF datasets: RGPS: Hutter, Nils (2019): 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 spacing from 1997 to 2008. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, PANGAEA, https://doi.org/10.1594/PANGAEA.909636 MOSAiC: Hutter, N. and von Albedyl, L. (in submission 2023): Linear Kinematic Features (leads & pressure ridges) detected and tracked in Sentinel-1 drift and deformation data during the MOSAiC expedition, PANGAEA MITgcm simulations: Hutter, N. et al. (2022). Linear Kinematic Feature detected and tracked in sea-ice deformation simulationed by all models participating in the Sea Ice Rheology Experiment and from RGPS (1.0) [Data set]. Zenodo. https://doi.org/10.5281/zenodo.6315226 References: Ringeisen, D., Hutter, N., and von Albedyl, L. (2023). Deformation lines in Arctic sea ice: intersection angles distribution and mechanical properties. The Cryosphere