On the Flow within the Transition Zone between Ice Sheet and Ice Shelf
作者： K. Herterich
DOI: 10.1007/978-94-009-3745-1_11
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摘要: The horizontal and vertical velocity components within the transition zone between ice sheet shelf are computed on a plane perpendicular to grounding line. flow is found numerically by solving non-linear elliptic differential equation with fixed boundary conditions. located around line its width of order thickness. In case basal sliding can be widened considerably.
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