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Gagliardini, O. et al. Capabilities and performance of Elmer/Ice, a new-generation ice sheet model.
GLIMMER is a fully coupled thermomechanical 3-dimensional ice sheet model with a sliding component.
"We cannot recreate six meters of sea level rise early in the Eemian without accounting for some brittle fracture in the ice sheet model," said DeConto.
Ice sheet model results thus constitute a new data set against which glacial geological information can be compared and tested.
These authors use an ice sheet model within a Bayesian statistical framework — in which critical processes are guided by expert synthesis — to simulate the mass loss from the entire Antarctic ice sheet to 2200.
We use an ice sheet model (GLIMMER) with an erosion component to examine the evolution of landscapes under ice sheets over long time scales in hypothetical situations.
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Telford and Geldart (1976) presented and described the forward modeling formula of 3D thin-sheet model, which is the basis for the inversion scheme developed here.
The β-sheet model and the non-homologous X-ray β-sheet ensemble exclude the variability between β-sheets in distinct proteins.
The investigations are within the framework of an axisymmetric geometry and the flame-sheet model.
That typically occurs in ice-sheet model simulations that involve more than about 2 m of sea-level-equivalent mass loss.
Mathematical formulations are given for the vortex-sheet model and the continuous mean flow model of the jet flow profiles.
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