Swath radar technology enables three-dimensional mapping of modern glacier beds over large areas at resolutions that are higher than those typically used in ice-flow models. These data may enable new understanding of processes at the ice-bed interface. Here, we use two densely surveyed swath-mapped topographies (<50 m2 resolution) of Thwaites Glacier to investigate the sensitivity of inferred basal friction proxies to bed roughness magnitude and orientation. Our work suggests that along-flow roughness influences inferred friction more than transverse-flow roughness, which agrees with analytic form-drag sliding theory. Using our model results, we calculate the slip length (the ratio of internal shear to basal slip). We find excellent agreeme...
The influence of basal disturbances on the steady state surface topography and on surface velocities...
The roughness of a glacier bed has high importance for the estimation of the sliding velocity and ca...
International audienceIn ice-sheet models, slip conditions at the base between the ice and the bed a...
Included in this handle are input data used in the inversions described in the paper "The impact of ...
International audienceResults of glacier flow models and associated estimates of future sea level ri...
Theoretical models predict that fast-flowing ice streams transmit information about their bedrock to...
Given high-resolution satellite-derived surface elevation and velocity data, ice-sheet models genera...
Given high-resolution satellite-derived surface elevation and velocity data, ice-sheet models genera...
Full Stokes flow-line models predict that fast-flowing ice streams transmit information about their ...
The influence of basal disturbances on the steady-state surface topography and on surface velocities...
Glacier basal sliding is a poorly understood aspect of glacier mechanics, and its spatial and tempor...
Large, complex stratigraphic folds that rise as high as 60% of the local ice thickness have been obs...
We use models constrained by remotely sensed data from Pine Island and Thwaites Glaciers, West Antar...
Transmission of basal variability to a glacier surface is investigated using analytical models for a...
The retreating Pine Island Glacier (PIG), West Antarctica, presently contributes ~5–10% of global se...
The influence of basal disturbances on the steady state surface topography and on surface velocities...
The roughness of a glacier bed has high importance for the estimation of the sliding velocity and ca...
International audienceIn ice-sheet models, slip conditions at the base between the ice and the bed a...
Included in this handle are input data used in the inversions described in the paper "The impact of ...
International audienceResults of glacier flow models and associated estimates of future sea level ri...
Theoretical models predict that fast-flowing ice streams transmit information about their bedrock to...
Given high-resolution satellite-derived surface elevation and velocity data, ice-sheet models genera...
Given high-resolution satellite-derived surface elevation and velocity data, ice-sheet models genera...
Full Stokes flow-line models predict that fast-flowing ice streams transmit information about their ...
The influence of basal disturbances on the steady-state surface topography and on surface velocities...
Glacier basal sliding is a poorly understood aspect of glacier mechanics, and its spatial and tempor...
Large, complex stratigraphic folds that rise as high as 60% of the local ice thickness have been obs...
We use models constrained by remotely sensed data from Pine Island and Thwaites Glaciers, West Antar...
Transmission of basal variability to a glacier surface is investigated using analytical models for a...
The retreating Pine Island Glacier (PIG), West Antarctica, presently contributes ~5–10% of global se...
The influence of basal disturbances on the steady state surface topography and on surface velocities...
The roughness of a glacier bed has high importance for the estimation of the sliding velocity and ca...
International audienceIn ice-sheet models, slip conditions at the base between the ice and the bed a...