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- W2011034246 abstract "A similarity solution of the equation that describes the time evolution of an ice sheet is obtained by separation of variables. It describes the motion of an initial δ function ice sheet distribution and is asymptotically stable with respect to all perturbations that leave the total volume invariant. Homogeneity in one horizontal direction is assumed." @default.
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- W2011034246 title "On the dynamics of the ice sheets" @default.
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- W2011034246 doi "https://doi.org/10.1029/jc086ic11p11065" @default.
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