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Efficient identification of ocean thermodynamics in a physical/biogeochemical ocean model with an iterative Importance Sampling method
Affiliation:1. Department of Land Resources and Environmental Sciences, Montana State University, 334 Leon Johnson Hall, Bozeman, MT 59717, USA;2. Montana Institute on Ecosystems, Montana State University, 605 Leon Johnson Hall, Bozeman, MT 59717, USA;3. Gianforte School of Computing, Montana State University, 357 Barnard Hall, Bozeman, MT 59717, USA;4. Department of Natural Resources and the Environment, University of Connecticut, 1376 Storrs Road, Unit 4087, Storrs, CT 06269, USA;5. Department of Biology, Duke University, Box 90338, Durham, NC 27708, USA;2. Provincial Mental Health Metabolic Program, BC Children’s Hospital, Vancouver, British Columbia, Canada;3. Children’s & Women’s Mental Health and Substance Use Services, Children’s and Women’s Health Centre of BC, Provincial Health Services Authority, Vancouver, British Columbia, Canada;4. Department of Psychiatry, University of British Columbia, Vancouver, British Columbia, Canada;5. BC Children’s Hospital, Provincial Health Services Authority, Vancouver, British Columbia, Canada
Abstract:Efficient identification of parameters in numerical models remains a computationally demanding problem. Here we present an iterative Importance Sampling approach and demonstrate its application to estimating parameters that control the heat uptake efficiency of a physical/biogeochemical ocean model coupled to a simple atmosphere. The algorithm has similarities to a previously-developed ensemble Kalman filtering (EnKF) method applied to similar problems, but is more flexible and powerful in the case of nonlinear models and non-Gaussian uncertainties. The method is somewhat more computationally demanding than the EnKF but may be preferred in cases where the approximations that the EnKF relies upon are unsound. Our results suggest that the three-dimensional structure of ocean tracer fields may act as a useful constraint on ocean mixing and consequently the heat uptake of the climate system under anthropogenic forcing.
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