Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
Mass loss from the Amundsen Sea Embayment of the West Antarctic Ice Sheet s?n nhà màu n?u ??t is a major contributor to global sea-level rise (SLR) and has been increasing over recent decades.Predictions of future SLR are increasingly modelled using ensembles of simulations within which model parameters and external forcings are varied within cre