MLOct 21, 2016

Mean-Field Variational Inference for Gradient Matching with Gaussian Processes

arXiv:1610.06949v11 citations
Originality Incremental advance
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This work addresses a specific computational bottleneck in ODE parameter inference for researchers in fields like systems biology or physics, offering an incremental improvement over sampling methods by making the problem analytically tractable for certain ODE types.

The paper tackles the problem of learning parameters of ordinary differential equations (ODEs) using gradient matching with Gaussian processes, where state variables are latent due to noise, by introducing a mean-field variational inference method that establishes analytically tractable and concave variational lower bounds for a restricted family of ODEs, enabling maximum a posteriori estimation and providing a proxy to the intractable posterior over state variables.

Gradient matching with Gaussian processes is a promising tool for learning parameters of ordinary differential equations (ODE's). The essence of gradient matching is to model the prior over state variables as a Gaussian process which implies that the joint distribution given the ODE's and GP kernels is also Gaussian distributed. The state-derivatives are integrated out analytically since they are modelled as latent variables. However, the state variables themselves are also latent variables because they are contaminated by noise. Previous work sampled the state variables since integrating them out is \textit{not} analytically tractable. In this paper we use mean-field approximation to establish tight variational lower bounds that decouple state variables and are therefore, in contrast to the integral over state variables, analytically tractable and even concave for a restricted family of ODE's, including nonlinear and periodic ODE's. Such variational lower bounds facilitate "hill climbing" to determine the maximum a posteriori estimate of ODE parameters. An additional advantage of our approach over sampling methods is the determination of a proxy to the intractable posterior distribution over state variables given observations and the ODE's.

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