In Situ Estimation of Erosion Model Parameters Using an Advection‐Diffusion Model and Bayesian Inversion
We describe a framework for the simultaneous estimation of model parameters in a partial differential equation using sparse observations. Markov Chain Monte Carlo sampling is used in a Bayesian framework to estimate posterior probability distributions for each parameter. We describe the necessary co...
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Published in | Journal of advances in modeling earth systems Vol. 15; no. 6 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Washington
John Wiley & Sons, Inc
01.06.2023
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Subjects | |
Online Access | Get full text |
ISSN | 1942-2466 1942-2466 |
DOI | 10.1029/2022MS003500 |
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Summary: | We describe a framework for the simultaneous estimation of model parameters in a partial differential equation using sparse observations. Markov Chain Monte Carlo sampling is used in a Bayesian framework to estimate posterior probability distributions for each parameter. We describe the necessary components of this approach and its broad potential for application in models of unsteady processes. The framework is applied to three case studies, of increasing complexity, from the field of cohesive sediment transport. We demonstrate that the framework can be used to recover posterior distributions for all parameters of interest and the results agree well with independent estimates (where available). We also demonstrate how the framework can be used to compare different model parameterizations and provide information on the covariance between model parameters.
Plain Language Summary
We describe a framework for the simultaneous estimation of multiple unobserved parameters by combining observations of a tracer with a numerical model. This framework uses Bayesian inference techniques established in statistical literature to estimate the unobserved parameters of interest used in the model with uncertainty quantification. We explain the key components of this framework in simple terms to encourage its use for analyzing other unsteady processes and performing quantitative inference on parameters that are difficult or impossible to measure directly. We then demonstrate the framework's efficacy by applying it to three case studies from the field of cohesive sediment transport that all use the transport equation (advection‐diffusion). Inferred parameter values show good agreement with independent estimates, where available.
Key Points
Probabilistic framework to estimate unobserved erosion model parameters using sparse measurements collected above the seabed
General approach can be updated with any model parameterization and quantitatively compared
The framework is applicable to many similar data sets with both unsteady or quasi‐steady forcing and response |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
ISSN: | 1942-2466 1942-2466 |
DOI: | 10.1029/2022MS003500 |