Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect heat loss and surface drag, but also provide insight into the underlying physics of sea ice deformation. Due to their elongated shape they are referred as Linear Kinematic Features (LKFs). This data-set includes LKFs that were detected and tracked in sea ice deformation simulated in an Arctic configuration of MITgcm using a 2-km horizontal grid spacing and an active 5-class ice thickness distribution. The model data is sampled for the entire observing period of the RADARSAT Geophysical Processor System (RGPS). The data-set spans the winter month (November to May) from 1997 to 2008 and covers the entire Arctic Ocean. A detailed description o...
Sea ice deforms constantly under the forcing of winds and ocean currents. Eventually the ice cover o...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
The Arctic sea ice deforms constantly due to stresses imposed by winds, ocean currents and interacti...
The sea-ice modelling community progresses towards Pan-Arctic simulations that explicitly resolve le...
Sea ice deforms constantly under the forcing of winds and ocean currents. Eventually the ice cover o...
Sea ice area and thickness have been on the decline in the Arctic over the past several decades. Und...
Simulating sea-ice drift and deformation in the Arctic Ocean is still a challenge because of the mul...
Simulating sea-ice drift and deformation in the Arctic Ocean is still a challenge because of the mul...
Code and data to reproduce the results presented in Ringeisen et al. (2023). The included notebooks ...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
Sea ice deforms constantly under the forcing of winds and ocean currents. Eventually the ice cover o...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
Leads and pressure ridges are dominant features of the Arctic sea ice cover. Not only do they affect...
The Arctic sea ice deforms constantly due to stresses imposed by winds, ocean currents and interacti...
The sea-ice modelling community progresses towards Pan-Arctic simulations that explicitly resolve le...
Sea ice deforms constantly under the forcing of winds and ocean currents. Eventually the ice cover o...
Sea ice area and thickness have been on the decline in the Arctic over the past several decades. Und...
Simulating sea-ice drift and deformation in the Arctic Ocean is still a challenge because of the mul...
Simulating sea-ice drift and deformation in the Arctic Ocean is still a challenge because of the mul...
Code and data to reproduce the results presented in Ringeisen et al. (2023). The included notebooks ...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
Sea ice deforms constantly under the forcing of winds and ocean currents. Eventually the ice cover o...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...
International audienceSimulating sea ice drift and deformation in the Arctic Ocean is still a challe...