REVIEW 3 major objections 6 minor 125 references
Automatic Differentiation-based Full Waveform Inversion with Flexible Workflows
T0 review · 3 major / 6 minor · reviewed 2026-08-12 · deepseek-v4-flash
Pith's one-line read The paper introduces ADFWI, an open-source automatic-differentiation framework that computes full waveform inversion gradients by backpropagation through the wave simulation, removing the need to derive adjoint equations and adjoint…
desk verdict A genuinely useful open-source AD-FWI workbench, but the 'robustness' headline outruns the synthetic evidence. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The central object is the computation graph of the staggered-grid finite-difference wave simulation, traversed in reverse by automatic differentiation. Each arithmetic operation in the forward modeling, from the initial wavefield through all time steps to the misfit evaluation, is recorded, and backpropagation applies the chain rule along this graph to produce gradients with respect to model parameters. This is what lets a single forward code act as its own adjoint, which is why new objective functions, regularizers, or neural-network reparameterizations can be added without deriving adjoint sources. Checkpointing the time axis and processing shots in mini-batches are the mechanisms that keep this graph's memory footprint manageable.
What would settle it
For each supported media and objective-function branch, compute the AD gradient on a small model and compare it against a central-difference gradient of the same objective; a mismatch in any branch, or a failed dot-product test between the forward operator and the AD-induced adjoint, would refute the claim of unified gradient correctness.
Extended reading notes
Core claim
The central claim is that automatic differentiation can serve as a complete replacement for the adjoint state method in full waveform inversion, provided the wave simulation is coded inside a differentiable computation graph. In this setup, the graph that produces synthetic seismograms also produces the gradient of any differentiable objective with respect to any model parameter, so the framework can support isotropic-acoustic, isotropic-elastic, and VTI/HTI elastic media without per-media adjoint derivations. The paper shows that objective functions such as soft-DTW and Wasserstein-Sinkhorn, whose adjoint sources are difficult to derive, are integrated simply by computing their scalar value and letting backpropagation handle the gradient. Synthetic tests on the Marmousi2 and Overthrust models, an elastic Marmousi2 test recovering both vp and vs, and a VTI anomaly test recovering both epsilon and delta, along with comparisons of objective functions, optimizers, regularizers, and neural-network reparameterization, are offered as evidence that the framework is practical and flexible.
Load-bearing premise
The framework's promise depends on backpropagation through the discretized finite-difference graph giving correct gradients for every wave equation and objective function it supports, but the paper directly validates this against central-difference gradients for only one isotropic-acoustic case.
Editorial extensions
If this is right
- Any differentiable misfit, including soft-DTW and Wasserstein-Sinkhorn, becomes immediately usable in FWI because the gradient is supplied by backpropagation rather than by an analytically derived adjoint source.
- The same inversion workflow applies across isotropic-acoustic, isotropic-elastic, and VTI/HTI elastic media, so multi-parameter inversions such as vp/vs or epsilon/delta can be run from one codebase.
- Neural-network reparameterization becomes a direct optimization route in which automatic differentiation updates the network weights, providing learned regularization and enabling fast dropout-based uncertainty estimates.
- Mini-batch shot processing and time-axis checkpointing reduce the memory overhead of automatic differentiation enough to make large-scale AD-based FWI practical on a single GPU.
- Because automatic differentiation differentiates through any smooth regularizer, the framework's support for total-variation and Tikhonov regularization extends by construction to future regularizers, since only the regularization value needs to be computed.
Reading between the lines
- If backpropagation is correct for every branch, FWI research shifts from deriving adjoints to implementing accurate forward physics, which should accelerate experimentation with viscoelastic attenuation, three-dimensional media, and other formulations that are currently expensive to derive by hand.
- The paper's direct gradient validation covers only one isotropic-acoustic case, so a natural stress test is to repeat the central-difference comparison for the elastic and VTI/HTI branches and for each non-L2 objective; a mismatch in any branch would silently corrupt those inversions.
- Dropout-based uncertainty should initially be read as a fast sensitivity indicator tied to the reparameterizing network architecture, not as a calibrated posterior; comparing it with ensemble inversions would clarify what the uncertainty maps measure.
- The same computation-graph convenience that makes total-variation and Tikhonov regularization trivial should extend to learned regularizers such as diffusion-model priors or dictionary transforms, though the paper only sketches this direction.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript presents ADFWI, an open-source PyTorch-based automatic-differentiation framework for full waveform inversion. The framework implements forward modeling for isotropic-acoustic, isotropic-elastic, and VTI/HTI-elastic media using staggered-grid finite differences with PML boundaries, and computes gradients by backpropagation rather than by hand-derived adjoint equations. It integrates seven objective functions, eight optimizers, Tikhonov/TV regularization, DNN-based model reparameterization with dropout uncertainty estimation, and memory-reduction strategies (mini-batching and checkpointing). The authors validate the framework on Marmousi2 and Overthrust acoustic tests, an elastic Marmousi2 test, a VTI anomaly test, objective-function and optimizer comparisons, and regularization/uncertainty demonstrations, concluding that ADFWI eliminates manual adjoint derivation and serves as a flexible workbench for FWI.
Significance. ADFWI is a substantial engineering contribution with clear practical value: the public repository and reproducible examples lower the barrier to experimenting with non-L2 misfits, anisotropic wave equations, and neural-network reparameterization. The systematic comparison of objective functions and optimizers under a common setup is useful. If the AD gradients are correct across all supported branches, the framework delivers on its central promise. However, the current evidence does not yet establish that correctness for the elastic, VTI/HTI, and non-L2 objective branches, and several evaluation choices (smoothed-true initial models, same-solver observed data) weaken the generality claims. The missing gradient verification is the main load-bearing gap.
major comments (3)
- [Section 2.2 and Supporting Figure S1] The only direct validation of the AD gradients is Supporting Figure S1, which compares AD gradients with finite-difference gradients for a single isotropic-acoustic experiment. No equivalent gradient check is reported for the ISO-elastic, VTI/HTI-elastic, or any non-L2 objective branch (envelope, global correlation, soft-DTW, Wasserstein-Sinkhorn), nor for the checkpointed or mini-batched computation graphs described in Section 4.3. Because AD differentiates the implemented forward code, a bug in the staggered-grid update, the Thomsen-to-stiffness mapping, the PML boundary, or the objective-function implementation would still yield low-misfit, visually plausible inversions when observed data are generated with the same forward solver. The paper's central claim in Section 5 that ADFWI 'eliminates the need for manual derivation and implementation of adjoint equations and sources' for all supported media and objectives therefore rests on an unverified branch. I request gradient checks (e.g., against finite differences or an adjoint-state reference, with a quantitative error metric) for at least one representative case in each wave-equation family and each objective-function family, or a correspondingly narrowed claim.
- [Section 3.1 and Table 1] All synthetic inversions start from initial models obtained by Gaussian smoothing of the true model (Table 1; Figures 3b, 4c-d, 6b), and all observed data are generated by the same forward solver used in inversion. The VTI test in Section 3.1.3 goes further: vp, vs, and rho are fixed at their true values, and only epsilon and delta are inverted from constant background values equal to the true background. These tests therefore demonstrate that the framework can refine a good starting model, but they do not independently confirm the correctness of the elastic/VTI forward modeling or the corresponding AD gradients, nor do they exercise the multi-parameter trade-offs that dominate practical elastic/anisotropic FWI. In addition, the HTI case advertised in the abstract and Section 2.1 is not exercised in any numerical test. I recommend adding at least one test with a non-trivial initial model (e.g., from travel-time tomography or a coarse model without smoothing the target) and, if possible, a dataset produced by an independent solver or with added noise, or alternatively stating this limitation explicitly and softening the generality claims in Sections 3.1.3 and 5.
- [Section 4.3] The checkpointing and mini-batch strategies modify the computation graph over which gradients are accumulated. The paper reports memory and runtime trade-offs but does not verify that the gradients obtained with checkpointing and gradient accumulation are identical (or acceptably close) to those from a full uncheckpointed backpropagation. Since a mismatch would introduce biased gradients and could silently degrade inversion quality, a gradient accuracy check (e.g., comparing checkpointed and uncheckpointed gradients on the Marmousi2 example) should be added before claiming that these strategies are 'practical for large-scale full waveform inversion' (Section 5).
minor comments (6)
- [Abstract; Section 2.3] Typos and naming inconsistencies should be corrected: 'forword modeling' in the abstract, 'Pytorch' in Section 2.3 and Figure 1 caption, and 'T-Distribution' in Section 2.3.1 should be 'PyTorch' and 'Student-t distribution'.
- [Section 3.1.3 / Figure 5] The text states that δ in the anomaly inclusions ranges from 0.1 to 0.25, while the Figure 5 caption states 0.1 to 0.3; these values should be harmonized.
- [Supporting Text S1, Eq. (7)] The sigmoid weighting expression is missing parentheses: it should read w(i) = 1/(1+exp(-(i - N/2))), and the text should state the value of N used in the WEC test in Section 4.1.
- [Section 2.3.1 / Table 2] The same objective is called 'Wasserstein-Sinkhorn' in Section 2.3.1 and 'Wasserstein Dist.' in Table 2; use one name consistently throughout.
- [Section 4.2] The dropout-based uncertainty maps are only qualitative; since no comparison with a reference uncertainty estimate (e.g., from multiple noise realizations or a Bayesian method) is provided, the claim of 'rapid estimation of uncertainty' should be accompanied by a caveat that the maps are uncalibrated.
- [Supporting Figure S1] The gradient check reports no quantitative error metric or the Δm used for the finite-difference reference; please add a normalized error or maximum-relative-error value.
Circularity Check
No circular derivation: ADFWI integrates standard components, and its tests are self-consistency checks rather than results reduced to inputs by construction.
full rationale
ADFWI is an engineering integration: the forward staggered-grid finite-difference propagators, objective functions, optimizers, and DNN reparameterization are standard components cited from external literature (e.g., Virieux 1986; Thomsen 1986; Cuturi & Blondel 2017; Kingma & Ba 2017). The central claim—that automatic differentiation replaces hand-derived adjoint sources—is a property of reverse-mode AD applied to the explicitly constructed computational graph, not a result defined in terms of the claim itself. The gradient validation in Supporting Figure S1 compares AD gradients with central-difference derivatives of the same discretized forward operator, which is an implementation-consistency check; it does not make the inversion results true by construction. The synthetic Marmousi2/Overthrust and VTI tests use data generated by the same forward solver and start from smoothed true models, so they are self-consistency benchmarks rather than independent predictions, but they do not reduce any claimed result to an input parameter or to a self-citation. The only self-citation (F. Liu et al., 2024) appears in a literature survey and is not load-bearing. No equation or result in the paper is equivalent to its inputs by construction.
Assumptions & free parameters
free parameters (4)
- Tikhonov/TV regularization weights alpha =
not reported
- Optimizer learning rates and adaptive-method hyperparameters =
not reported
- WEC weighting schedule parameter N =
not reported
- CNN architecture and training choices for DNN reparameterization =
2-5 blocks, latent 100, 4x4 kernels, channel counts 4-256, LeakyReLU 0.1, dropout p=0.1/0.2
assumptions (5)
- domain assumption The staggered-grid finite-difference propagators used in ADFWI accurately solve the acoustic and elastic wave equations for the tested 2D scenarios.
- domain assumption Backpropagation through the discretized simulation graph yields gradients equivalent to adjoint-state gradients for all implemented media and objective functions.
- domain assumption Synthetic observed data generated with the same propagator used in inversion constitute a valid test of FWI framework behavior.
- domain assumption For the VTI test, fixing the true vp, vs, and rho models while inverting only epsilon and delta does not bias the assessment of crosstalk.
- domain assumption PyTorch optimizer implementations with user-tuned hyperparameters produce behavior representative of each method's general performance.
Cite this review
Pith. "Pith review of Automatic Differentiation-based Full Waveform Inversion with Flexible Workflows." pith.science (2026). https://pith.science/paper/DFG5LDAP
@misc{pith2026241200486,
author = {Pith},
title = {Pith review of: Automatic Differentiation-based Full Waveform Inversion with Flexible Workflows},
year = {2026},
howpublished = {\url{https://pith.science/paper/DFG5LDAP}},
note = {Machine review of arXiv:2412.00486}
}
read the original abstract
Full waveform inversion (FWI) is able to construct high-resolution subsurface models by iteratively minimizing discrepancies between observed and simulated seismic data. However, its implementation can be rather involved for complex wave equations, objective functions, or regularization. Recently, automatic differentiation (AD) has proven to be effective in simplifying solutions of various inverse problems, including FWI. In this study, we present an open-source AD-based FWI framework (ADFWI), which is designed to simplify the design, development, and evaluation of novel approaches in FWI with flexibility. The AD-based framework not only includes forword modeling and associated gradient computations for wave equations in various types of media from isotropic acoustic to vertically or horizontally transverse isotropic elastic, but also incorporates a suite of objective functions, regularization techniques, and optimization algorithms. By leveraging state-of-the-art AD, objective functions such as soft dynamic time warping and Wasserstein distance, which are difficult to apply in traditional FWI are also easily integrated into ADFWI. In addition, ADFWI is integrated with deep learning for implicit model reparameterization via neural networks, which not only introduces learned regularization but also allows rapid estimation of uncertainty through dropout. To manage high memory demands in large-scale inversion associated with AD, the proposed framework adopts strategies such as mini-batch and checkpointing. Through comprehensive evaluations, we demonstrate the novelty, practicality and robustness of ADFWI, which can be used to address challenges in FWI and as a workbench for prompt experiments and the development of new inversion strategies.
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