The longitudinal velocity and thickness of an ice shelf in steady plane flow, when temperature is prescribed as a function of the spatial coordinates, are determisned by simultaneous integro-differential equations. These are solved numerically to illustrate the effects of temperature distribution, depth and ice flux at the grounding line, and surface accumulation. -from Current Antarctic Literature
CITATION STYLE
Morland, L. W., & Zainuddin, R. (1987). Plane and radial ice-shelf flow with prescribed temperature profile. Dynamics of the West Antarctic Ice Sheet, 117–140. https://doi.org/10.1007/978-94-009-3745-1_7
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