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ziyiyin97 committed Mar 14, 2024
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4 changes: 2 additions & 2 deletions _quarto.yml
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Expand Up @@ -18,8 +18,8 @@ website:
contents:
- file: DigitalTwin/abstract.qmd
text: "Digital twin with control"
- file: WISER/paper.qmd
text: "Full-waveform variational inference"
- file: yin2024SEG/paper.qmd
text: "WISER: full-Waveform variational Inference via Subsurface Extensions with Refinements"
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center:
- file: license.qmd
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2 changes: 1 addition & 1 deletion index.qmd
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Expand Up @@ -10,4 +10,4 @@ List of abstrac:

- [Digital twin with control](DigitalTwin/abstract.qmd) An uncertainty-aware digital twin for geological carbon storage

- [WISER](WISER/paper.qmd): full-Waveform variational Inference via Subsurface Extensions with Refinements
- [WISER](yin2024SEG/paper.qmd): full-Waveform variational Inference via Subsurface Extensions with Refinements
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32 changes: 30 additions & 2 deletions WISER/paper.qmd → yin2024SEG/paper.qmd
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Expand Up @@ -14,7 +14,7 @@ We introduce a cost-effective Bayesian inference method for full-waveform invers

## Amortized variational inference

Our method concerns estimation of migration-velocity models from noisy seismic data through the inversion of the wave modeling operator. Instead of seeking only a single velocity model, our method aims to draw samples from the posterior distribution of migration-velocity models conditioned on the observed shot data. In this context, we train conditional normalizing flows (CNFs) to approximate this posterior distribution. To simply the mapping between seismic image and shot data, we use common-image gathers (CIGs) as an information-preserving physics-informed summary statistics to embed the shot data, and then train the CNFs on pairs of velocity models and CIGs [@yin2023wise]. After training, the inverse of CNF turns random realizations of the standard Gaussian distribution into posterior samples (velocity models) conditioned on any seismic observation that is in the same statistical distribution as the training data, shown in the upper part of the flowchart.
Our method concerns estimation of migration-velocity models from noisy seismic data through the inversion of the wave modeling operator. Instead of seeking only a single velocity model, our method aims to draw samples from the posterior distribution of migration-velocity models conditioned on the observed shot data. In this context, we train conditional normalizing flows (CNFs) to approximate this posterior distribution. To simply the mapping between seismic image and shot data, we use common-image gathers (CIGs) as an information-preserving physics-informed summary statistics to embed the shot data, and then train the CNFs on pairs of velocity models and CIGs. After training, the inverse of CNF turns random realizations of the standard Gaussian distribution into posterior samples (velocity models) conditioned on any seismic observation that is in the same statistical distribution as the training data, shown in the upper part of the flowchart. We term this amortized inference framework WISE, short for full-**W**aveform variational **I**nference via **S**ubsurface **E**xtensions [@yin2023wise]. We further propose a physics-based **R**efinment approach to make it WISER.

## Physics-based refinement

Expand All @@ -24,7 +24,35 @@ While the trained amortized CNF can generate posterior velocity samples instanta

To understand how the uncertainty in the migration-velocity models propagates to imaged reflectors, forward uncertainty is assessed by carrying out high-frequency imaging for different posterior velocity samples, shown on the right-hand side of the flowchart. The uncertainty in the imaged reflectors is revealed in variance in both the amplitude and the positioning of the reflectors.

![](./figs/WISER-workflow.pdf){width=99%}
::: {#fig-workflow}
![](./figs/WISER-workflow.jpeg){width=99%}

WISER workflow.
:::

::: {#fig-wise-vs-wiser layout="[[49, 49], [49, 49], [49, 49], [49, 49], [49, 49]]"}
![](./figs/background-colorbar.png){#fig-background}

![](./figs/true-v-colorbar.png){#fig-true}

![](./figs/WISE-v-3D.png){#fig-wise-v-3d}

![](./figs/WISER-v-3D.png){#fig-wiser-v-3d}

![](./figs/WISE-UQ-v.png){#fig-wise-uq}

![](./figs/WISER-UQ-v.png){#fig-wiser-uq}

![](./figs/WISE-rtm-3D.png){#fig-wise-cm-rtm}

![](./figs/WISER-rtm-3D.png){#fig-wiser-cm-rtm}

![](./figs/WISE-UQ-rtm.png){#fig-wise-uq-rtm}

![](./figs/WISER-UQ-rtm.png){#fig-wiser-uq-rtm}

*(a)* 1D initial velocity model; *(b)* unseen ground truth velocity model; *(c)* Estimated migration-velocity models from WISE; *(e)* point-wise standard deviation of the migration-velocity models from WISE; *(g)* imaged reflectivities using migration-velocity models from WISE; *(i)* point-wise standard deviation of the imaged reflectivities from WISE; *(d)(f)(h)(j)* are the counterparts of *(c)(e)(g)(i)* but from WISER.
:::

## References

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