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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Main Authors: Phipps, Steven J., Roberts, Jason L., King, Matt A.
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2020
Subjects:
Online Access:https://doi.org/10.5281/zenodo.4275053
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spelling ftzenodo:oai:zenodo.org:4275053 2024-09-15T17:41:39+00:00 An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3 Phipps, Steven J. Roberts, Jason L. King, Matt A. 2020-11-16 https://doi.org/10.5281/zenodo.4275053 unknown Zenodo https://doi.org/10.5281/zenodo.4275052 https://doi.org/10.5281/zenodo.4275053 oai:zenodo.org:4275053 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Geoscientific model Parameterisation Parameter uncertainty Parameter optimisation Parallel Ice Sheet Model (PISM) Antarctic Ice Sheet Large ensemble modelling info:eu-repo/semantics/other 2020 ftzenodo https://doi.org/10.5281/zenodo.427505310.5281/zenodo.4275052 2024-07-27T07:16:40Z 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 the 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. Other/Unknown Material Antarc* Antarctic Ice Sheet Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Geoscientific model
Parameterisation
Parameter uncertainty
Parameter optimisation
Parallel Ice Sheet Model (PISM)
Antarctic Ice Sheet
Large ensemble modelling
spellingShingle Geoscientific model
Parameterisation
Parameter uncertainty
Parameter optimisation
Parallel Ice Sheet Model (PISM)
Antarctic Ice Sheet
Large ensemble modelling
Phipps, Steven J.
Roberts, Jason L.
King, Matt A.
An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
topic_facet Geoscientific model
Parameterisation
Parameter uncertainty
Parameter optimisation
Parallel Ice Sheet Model (PISM)
Antarctic Ice Sheet
Large ensemble modelling
description 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 the 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.
format Other/Unknown Material
author Phipps, Steven J.
Roberts, Jason L.
King, Matt A.
author_facet Phipps, Steven J.
Roberts, Jason L.
King, Matt A.
author_sort Phipps, Steven J.
title An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
title_short An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
title_full An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
title_fullStr An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
title_full_unstemmed An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
title_sort iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the parallel ice sheet model (pism) version 0.7.3
publisher Zenodo
publishDate 2020
url https://doi.org/10.5281/zenodo.4275053
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_relation https://doi.org/10.5281/zenodo.4275052
https://doi.org/10.5281/zenodo.4275053
oai:zenodo.org:4275053
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.427505310.5281/zenodo.4275052
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