2026 study: automatic viscoelastic Earth adjoints
Research context
development · conditional · As of 2026-10-10
peer reviewed · 2026-04-10
- Study design
- Forward/adjoint finite-element framework tested against analytical and numerical benchmarks and synthetic Earth-like inversions.
- Reported result
- Automatic gradients support joint ice-loading and mantle-viscosity optimization, including lateral viscosity and alternative rheologies.
- Limitations
- Synthetic demonstrations do not identify a unique real loading history or resolve competing transient-rheology explanations.
Scott et al. extended G-ADOPT to elastic-compressible, laterally variable and non-Maxwell viscoelastic models.
Key knowledge
Scott et al. extended G-ADOPT to elastic-compressible, laterally variable and non-Maxwell viscoelastic models. Analytical/numerical benchmarks and synthetic inversions demonstrate computational capability to recover prescribed ice histories and viscosity structure, rather than a uniquely verified real Earth history.
Conditions and scope
- Published 10 April 2026; selected methods, benchmarks and conclusion inspected.
- Synthetic truth recovery and real-data uncertainty are separate validation tasks.
Sources · 1
References
Sources retain their recorded scope. A source link alone does not establish verification of every statement.
Evidence and review
Automated forward and adjoint modelling of viscoelastic deformation of the solid Earth: Sections 2–4 and conclusion: rheologies, benchmarks, synthetic inversions (selected source body inspected).
2026-10-10 · Bounded source check of the recorded statement and conditions. This does not certify a unique physical model, reproduce the cited study or replace independent branch review.
Entry details
Permanent link to this entry ↗- Record identity
- research-earth-gia-2026-study
- Revision
- research.1.editorial-precision-20261011.1
- Structured reference record
- Postgraduate & research reference