The aim of this work is to develop a numerical method to solve a moving bou
ndary problem governed by a time dependent nonlinear convection-diffusion e
quation. The mathematical formulation can be framed as a nonlinear paraboli
c complementarity problem. The model has recently been used to compute ice
sheet profiles in theoretical glaciology. After describing the mathematical
model of the ice sheet motion and the corresponding dimensionless equation
s, the proposed numerical method involves an upwind scheme for time semidis
cretization, fixed point method for the nonlinear diffusion term, finite el
ements approximation in space and a duality type algorithm for solving the
obstacle like problem at each step.
Finally, several numerical simulation examples involving real data sets iss
ued from the Antarctic ice sheet are shown.