Ice sheet flow with thermally activated sliding. Part 1: the role of advection

DOI10.1098/rspa.2019.0410zbMath1472.86038OpenAlexW2981723416WikidataQ91315850 ScholiaQ91315850MaRDI QIDQ5160792

M. Haseloff, C. Schoof, Elisa Mantelli

Publication date: 29 October 2021

Published in: Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1098/rspa.2019.0410

zbMATH Keywords

mathematical modellingfluid mechanicsglaciologypremeltingbasal slidingice streamthermo-mechanical feedbacksthermo-mechanical ice sheet model

Mathematics Subject Classification ID

PDEs in connection with fluid mechanics (35Q35) Glaciology (86A40) Forced convection (76R05) PDEs in connection with geophysics (35Q86)

Related Items (2)

Lubricated axisymmetric gravity currents of power-law fluids ⋮ Ice sheet flow with thermally activated sliding. Part 2: the stability of subtemperate regions

Cites Work

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• A boundary layer model for ice stream margins
• Thermally driven migration of ice-stream shear margins
• Marine ice-sheet dynamics. Part 1. The case of rapid sliding
• Stability of ice-sheet grounding lines
• Thin-Film Flows with Wall Slip: An Asymptotic Analysis of Higher Order Glacier Flow Models
• A sliding law for glaciers of constant viscosity in the presence of subglacial cavitation
• A theoretical treatment of the sliding of glaciers in the absense of cavitation
• On a Doubly Nonlinear Parabolic Obstacle Problem Modelling Ice Sheet Dynamics
• Thermoviscous stability of ice-sheet flows
• Subglacial hydrology and the formation of ice streams
• PREMELTING DYNAMICS

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