LGJan 17, 2024

Data Attribution for Diffusion Models: Timestep-induced Bias in Influence Estimation

arXiv:2401.09031v313 citationsh-index: 5Trans. Mach. Learn. Res.
Originality Incremental advance
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This work addresses the problem of interpreting 'black-box' diffusion models for researchers and practitioners, though it is incremental as it adapts existing frameworks to a specific model type.

The paper tackled the challenge of attributing diffusion model outputs to training data by identifying timestep-induced bias in influence estimation, and introduced a re-normalized method that reduced generally influential samples to one-third of the original quantity.

Data attribution methods trace model behavior back to its training dataset, offering an effective approach to better understand ''black-box'' neural networks. While prior research has established quantifiable links between model output and training data in diverse settings, interpreting diffusion model outputs in relation to training samples remains underexplored. In particular, diffusion models operate over a sequence of timesteps instead of instantaneous input-output relationships in previous contexts, posing a significant challenge to extend existing frameworks to diffusion models directly. Notably, we present Diffusion-TracIn that incorporates this temporal dynamics and observe that samples' loss gradient norms are highly dependent on timestep. This trend leads to a prominent bias in influence estimation, and is particularly noticeable for samples trained on large-norm-inducing timesteps, causing them to be generally influential. To mitigate this effect, we introduce Diffusion-ReTrac as a re-normalized adaptation that enables the retrieval of training samples more targeted to the test sample of interest, facilitating a localized measurement of influence and considerably more intuitive visualization. We demonstrate the efficacy of our approach through various evaluation metrics and auxiliary tasks, reducing the amount of generally influential samples to $\frac{1}{3}$ of its original quantity.

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