An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3

Physical processes within geoscientific models are sometimes described by simplified schemes known as parameterisations. The values of the parameters within these schemes can be poorly constrained by theory or observation. Uncertainty in the parameter values translates into uncertainty in the output...

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Bibliographic Details
Published in:Geoscientific Model Development
Main Authors: Phipps, SJ, Roberts, JL, King, MA
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2021
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Online Access:https://eprints.utas.edu.au/37072/
https://eprints.utas.edu.au/37072/1/146031%20-%20An%20iterative%20process%20for%20efficient%20optimisation%20of%20parameters%20in%20geoscientific%20models.pdf
Description
Summary:Physical processes within geoscientific models are sometimes described by simplified schemes known as parameterisations. The values of the parameters within these schemes can be poorly constrained by theory or observation. Uncertainty in the parameter values translates into uncertainty in the outputs of the models. Proper quantification of the uncertainty in model predictions therefore requires a systematic approach for sampling parameter space. In this study, we develop a simple and efficient approach to identify regions of multi-dimensional parameter space that are consistent with observations. Using the Parallel Ice Sheet Model to simulate the present-day state of the Antarctic Ice Sheet, we find that co-dependencies between parameters preclude any simple identification of a single optimal set of parameter values. Approaches such as large ensemble modelling are therefore required in order to generate model predictions that incorporate proper quantification of the uncertainty arising from the parameterisation of physical processes.