Inference of the bottom topography in anisothermal mildly-sheared shallow ice flows
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Publication:1987945
DOI10.1016/J.CMA.2019.01.003zbMath1440.86010OpenAlexW2913447677WikidataQ128439382 ScholiaQ128439382MaRDI QIDQ1987945
Publication date: 16 April 2020
Published in: Computer Methods in Applied Mechanics and Engineering (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.cma.2019.01.003
Related Items (3)
Covariance kernels investigation from diffusive wave equations for data assimilation in hydrology ⋮ Physically-constrained data-driven inversions to infer the bed topography beneath glaciers flows. Application to East Antarctica ⋮ An augmented Lagrangian algorithm for recovery of ice thickness in unidirectional flow using the shallow ice approximation
Uses Software
Cites Work
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- Inverse problems in free surface flows: a review
- Mathematical geoscience
- Iterative regularization methods for nonlinear ill-posed problems
- Inverse rheometry and basal properties inference for pseudoplastic geophysical flows
- Multi-regime shallow free surface laminar flow models for quasi-Newtonian fluids
- Thin-Film Flows with Wall Slip: An Asymptotic Analysis of Higher Order Glacier Flow Models
- Gmsh: A 3-D finite element mesh generator with built-in pre- and post-processing facilities
- Thermomechanical balances of ice sheet flows
- Inference of the bottom properties in shallow ice approximation models
- Asymptotic Theories of Ice Sheets and Ice Shelves
- Inverse Problem Theory and Methods for Model Parameter Estimation
- Estimating the ice thickness of mountain glaciers with an inverse approach using surface topography and mass-balance
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