Steady plane flow of ice sheets over lar
β
L. W. Morland; A. Draghicescu
π
Article
π
1998
π
John Wiley and Sons
π
English
β 326 KB
The reduced model for a large ice sheet Β―ow is uniformly valid when the bed topography is Β―at or has slopes relative to the horizontal no greater than order e, where e 2 is a very small dimensionless viscosity based on the geometry and Β―ow parameters. Real beds will have much greater slopes, of orde