2018
DOI: 10.48550/arxiv.1808.01084
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A Bayesian Approach to Estimating Background Flows from a Passive Scalar

Abstract: We consider the statistical inverse problem of estimating a background flow field (e.g., of air or water) from the partial and noisy observation of a passive scalar (e.g., the concentration of a solute), a common experimental approach to visualizing complex fluid flows. Here the unknown is a vector field that is specified by a large or infinite number of degrees of freedom. Since the inverse problem is ill-posed, i.e., there may be many or no background flows that match a given set of observations, we adopt a … Show more

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Cited by 5 publications
(12 citation statements)
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“…Having formulated our mixing result for the exact HMC algorithm associated with (1.1) we would like to be able to demonstrate that the conditions (1.6)-(1.7) which we impose on the potential U can be verified in concrete examples specifically as would apply to the Bayesian approach to PDE inverse problems. Here, as an illustrative example, we consider the problem of recovering a divergence free fluid flow q from the sparse and noisy observation of a passive solute θ(q) as was recently studied in [BGHK18,BGHK19].…”
Section: Overview Of the Main Resultsmentioning
confidence: 99%
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“…Having formulated our mixing result for the exact HMC algorithm associated with (1.1) we would like to be able to demonstrate that the conditions (1.6)-(1.7) which we impose on the potential U can be verified in concrete examples specifically as would apply to the Bayesian approach to PDE inverse problems. Here, as an illustrative example, we consider the problem of recovering a divergence free fluid flow q from the sparse and noisy observation of a passive solute θ(q) as was recently studied in [BGHK18,BGHK19].…”
Section: Overview Of the Main Resultsmentioning
confidence: 99%
“…In order to place (1.11) in a rigorous functional setting we adapt some results from [BGHK19,BGHK18]. In view of (8.3), (8.4) we consider a slightly more general version of (1.9) where we include an external forcing term f : [0, T ] × T 2 → R, namely,…”
Section: Mathematical Setting Of the Advection Diffusion Equation Ass...mentioning
confidence: 99%
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