Inference of the bottom properties in shallow ice approximation models
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Publication:4597557
DOI10.1088/1361-6420/aa7b92zbMath1375.86017OpenAlexW2594583905MaRDI QIDQ4597557
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Publication date: 13 December 2017
Published in: Inverse Problems (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1088/1361-6420/aa7b92
Related Items (4)
Bedrock reconstruction from free surface data for unidirectional glacier flow with basal slip ⋮ Physically-constrained data-driven inversions to infer the bed topography beneath glaciers flows. Application to East Antarctica ⋮ Inference of the bottom topography in anisothermal mildly-sheared shallow ice flows ⋮ An augmented Lagrangian algorithm for recovery of ice thickness in unidirectional flow using the shallow ice approximation
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Cites Work
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- Inverse problems in free surface flows: a review
- Mathematical geoscience
- Effective boundary condition at a rough surface starting from a slip condition
- Automated solution of differential equations by the finite element method. The FEniCS book
- Inverse rheometry and basal properties inference for pseudoplastic geophysical flows
- Multi-regime shallow free surface laminar flow models for quasi-Newtonian fluids
- Steady, Shallow Ice Sheets as Obstacle Problems: Well-Posedness and Finite Element Approximation
- Thin-Film Flows with Wall Slip: An Asymptotic Analysis of Higher Order Glacier Flow Models
- Thermomechanical balances of ice sheet flows
- The Use of the L-Curve in the Regularization of Discrete Ill-Posed Problems
- Estimating the ice thickness of mountain glaciers with an inverse approach using surface topography and mass-balance
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