Evaluates the ability of quantum and classical models to perform full-waveform inversion (FWI) by predicting subsurface velocity maps from scaled seismic waveform data. It probes the effectiveness of physics-guided data scaling and layer-wise variational quantum circuit designs in geophysical imaging tasks. Use when the user wants to benchmark on FlatVelA, or asks about evaluating this task. Reports SSIM.
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---
name: flatvela-fwi-eval
description: Evaluates the ability of quantum and classical models to perform full-waveform inversion (FWI) by predicting subsurface velocity maps from scaled seismic waveform data. It probes the effectiveness of physics-guided data scaling and layer-wise variational quantum circuit designs in geophysical imaging tasks. Use when the user wants to benchmark on FlatVelA, or asks about evaluating this task. Reports SSIM.
metadata:
skill_kind: dataset_eval
source_arxiv: 2311.12333
bibtex_key: jiang2023qugeo
confidence: high
---
# flatvela-fwi-eval
> QuGeo: An End-to-end Quantum Learning Framework for Geoscience -- A Case Study on Full-Waveform Inversion — Jiang et al. (2023) (arXiv:2311.12333, 2023)
## What this evaluates
Evaluates the ability of quantum and classical models to perform full-waveform inversion (FWI) by predicting subsurface velocity maps from scaled seismic waveform data. It probes the effectiveness of physics-guided data scaling and layer-wise variational quantum circuit designs in geophysical imaging tasks.
## Datasets
- **FlatVelA** — total 500; splits: train (400), test (100)
## Metrics
- `SSIM` **(primary)** — range: [0, 1]
- Structural Similarity Image Metric, measuring perceptual similarity between predicted and ground-truth velocity maps. Values closer to 1 indicate higher similarity.
- `MSE` — range: other
- Mean Squared Error, calculating the average squared difference between predicted and true velocity values.
## Input / output format
**Input**: Scaled seismic waveform data (dimension 256) for inference; scaled seismic data and ground-truth 8x8 velocity maps for training.
**Output**: Predicted 8x8 velocity map.
## Scoring recipe
```python
For each of the 100 test samples:
pred = model(input_seismic_data)
ssim_val = compute_ssim(pred, ground_truth_velocity_map)
mse_val = compute_mse(pred, ground_truth_velocity_map)
Return mean(ssim_val) and mean(mse_val) across the test set.
```
## Common pitfalls
- Naive downsampling (D-Sample) loses critical physical information, drastically degrading SSIM/MSE compared to physics-guided or CNN-based scaling.
- Models must be compared with matched parameter counts; quantum and classical baselines differ by only 40-60 parameters.
- Metrics are computed on the downsampled 8x8 velocity maps, not the original 70x70 resolution, so absolute error magnitudes are scale-dependent.
## Evidence (verbatim from paper)
> To support training, we split the FlatVelA dataset with 500 samples into a training set (size of 400) and a test set (size of 100). Figure 5(a) is a VQC model obtained in training, where the x-axis and y-axis stand for Structural Similarity Image Metric (SSIM) and Mean Squared Error (MSE), respectively.
## Citation
```bibtex
@misc{jiang2023qugeo,
title={QuGeo: An End-to-end Quantum Learning Framework for Geoscience -- A Case Study on Full-Waveform Inversion},
author={Jiang et al. (2023)},
year={2023},
note={arXiv:2311.12333}
}
```
- arXiv: 2311.12333