heleneseroussi
Thank you for the clarification. How does refreezing work in the model then?
Additionally, can you also talk a bit about water fraction in the model, for example, its physical basis and application? When trying to parameterize the basal friction for some paleo ice-sheets, I am thinking whether the water fraction output might provide some kind of indicator of basal sliding. Or do you think I should simply look at the temperature of the bottom layer?