The compressible adjoint equations in geodynamics: derivation and numerical assessment
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Publication:284442
DOI10.1007/S13137-016-0080-5zbMath1345.86003OpenAlexW2335071651MaRDI QIDQ284442
Hans-Peter Bunge, Siavash Ghelichkhan
Publication date: 18 May 2016
Published in: GEM - International Journal on Geomathematics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/s13137-016-0080-5
Inverse problems in geophysics (86A22) Computational methods for problems pertaining to geophysics (86-08)
Related Items (4)
Adjoint-based inversion for porosity in shallow reservoirs using pseudo-transient solvers for non-linear hydro-mechanical processes ⋮ A semi-analytic accuracy benchmark for Stokes flow in 3-D spherical mantle convection codes ⋮ Multi-physics adjoint modeling of Earth structure: combining gravimetric, seismic, and geodynamic inversions ⋮ The adjoint equations for thermochemical compressible mantle convection: derivation and verification by twin experiments
Cites Work
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- The adjoint method in geodynamics: derivation from a general operator formulation and application to the initial condition problem in a high resolution mantle circulation model
- Restoring past mantle convection structure through fluid dynamic inverse theory: regularisation through surface velocity boundary conditions
- The adjoint method in seismology
- The adjoint method in seismology—
- Numerical simulations of mantle convection: Time-dependent, three-dimensional, compressible, spherical shell
- Convection in a compressible fluid with infinite Prandtl number
- Convection in the earth's mantle: towards a numerical simulation
- Function minimization by conjugate gradients
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