Bayesian full waveform inversion using the shifted ordinary differential equation method with underdamped Langevin Markov chain Monte Carlo

Clicks: 2
ID: 324936
2026
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal

Ranked #64 of 215 articles by views in geophysical journal international

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 215 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract
Summary Full waveform inversion (FWI) is a powerful tool for constructing high-resolution subsurface models but remains fundamentally ill-posed due to sparse and noisy data, modeling errors, and the severe nonlinearity of the forward modeling. Because this inherent nonlinearity creates complex uncertainty structures that traditional deterministic optimization cannot easily resolve. To fully quantify this inversion uncertainty and explore all plausible solutions, Bayesian FWI seeks to sample directly from the posterior probability density function using Markov chain Monte Carlo (MCMC) algorithms. However, traditional MCMC methods suffer from inefficient exploration (poor mixing) in high-dimensional model spaces. In this study, we adopt an efficient sampler based on underdamped Langevin diffusion (ULD). The stochastic differential equation (SDE) governing ULD is approximated using the shifted ordinary differential equation (ODE) method, which converts the stochastic dynamics into a deterministic ODE that is easier to solve numerically. Building on this formulation, we introduce the SORT (Shifted ODE with Runge–Kutta Three) sampling method. The SORT method employs a third-order Runge-Kutta scheme to discretize the ODE, which effectively reduces discretization errors and enables highly efficient sampling. We validate the performance of SORT through synthetic 2D acoustic FWI experiments in both low- and high-dimensional model spaces. The numerical results show that SORT efficiently explores high-dimensional posterior distributions and produces stable and reliable mean and uncertainty estimates for complex subsurface structures.
Reference Key
openalex_W7202342443 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Shuang Wang, Xiangbo Gong, Qiao Cheng, Guangshuai Peng
Journal geophysical journal international
Year 2026
DOI
10.1093/gji/ggag318
URL
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.