Inverse method for sliding coefficients at Vestfonna ice cap
In a recent publication in The Cryosphere Schäfer et al. use a Robin inverse method to infer the basal friction from the surface velocities observed in 1995 for the Vestfonna ice cap on Svalbard. The results demonstrate that especially the ice caps on Nordaustlandet, with their mixture of static central parts and fast moving outlet glaciers, demand the correct spatial distribution of sliding coefficients and that - in lack of a complete understanding of the physics taking place at the bedrock - inverse models for the time being are the only means to deliver that spatial distribution. Further investigations of comparison of sliding coefficients obtained for datasets taken at different times shall shed further light on the nature of the sliding underneath Vestfonna ice cap.