Dimension reduction in the Bayesian analysis of a numerical climate model

We present a prediction of the strength of the meridional overturning circulation (MOC) in the Atlantic Ocean during the 21st century, and a quantitative estimate of its uncertainty. The MOC has been suggested as a potential source of abrupt climate change, with the ability to alter the climate of t...

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Main Author: McNeall, Douglas James
Format: Thesis
Language:English
Published: 2008
Subjects:
Online Access:https://eprints.soton.ac.uk/69028/
https://eprints.soton.ac.uk/69028/1/McNeall_2008_PhD.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:69028 2023-07-30T04:05:31+02:00 Dimension reduction in the Bayesian analysis of a numerical climate model McNeall, Douglas James 2008 text https://eprints.soton.ac.uk/69028/ https://eprints.soton.ac.uk/69028/1/McNeall_2008_PhD.pdf en eng https://eprints.soton.ac.uk/69028/1/McNeall_2008_PhD.pdf McNeall, Douglas James (2008) Dimension reduction in the Bayesian analysis of a numerical climate model. University of Southampton, Faculty of Engineering Science and Mathematics, School of Ocean and Earth Science, Doctoral Thesis, 176pp. Thesis NonPeerReviewed 2008 ftsouthampton 2023-07-09T21:06:26Z We present a prediction of the strength of the meridional overturning circulation (MOC) in the Atlantic Ocean during the 21st century, and a quantitative estimate of its uncertainty. The MOC has been suggested as a potential source of abrupt climate change, with the ability to alter the climate of the North Atlantic on a short time-scale. The prediction takes the form of a calibrated uncertainty analysis, combining observations of the MOC, an ensemble of runs from a climate model, and expert knowledge, in a Bayesian fashion. Uncertainty in model behaviour due to the model structure and forcing is explored by running an ensemble of the Earth system model of intermediate complexity GENIE-1. Input parameters representing physical constants, simplified processes, and forcings are varied across the ensemble in a designed computer experiment. We develop quantitative and qualitative methods to compare observational data of the MOC with corresponding output from the ensemble, to learn about plausible input configurations of the model. Dimension reduction is used to express patterns of variation in model behaviour across the ensemble in a low-dimensional form. The ensemble is used to train an emulator; a fast statistical approximation to the expensive model, that includes an estimate of uncertainty due to the limited size of the ensemble. By training the emulator using the low-dimensional representations of the output, we are able to predict high-dimensional model output at input configurations not tested in the original ensemble. This allows a more complete expression of the uncertainty in the evolution of the MOC throughout the 21st century. Thesis North Atlantic University of Southampton: e-Prints Soton
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description We present a prediction of the strength of the meridional overturning circulation (MOC) in the Atlantic Ocean during the 21st century, and a quantitative estimate of its uncertainty. The MOC has been suggested as a potential source of abrupt climate change, with the ability to alter the climate of the North Atlantic on a short time-scale. The prediction takes the form of a calibrated uncertainty analysis, combining observations of the MOC, an ensemble of runs from a climate model, and expert knowledge, in a Bayesian fashion. Uncertainty in model behaviour due to the model structure and forcing is explored by running an ensemble of the Earth system model of intermediate complexity GENIE-1. Input parameters representing physical constants, simplified processes, and forcings are varied across the ensemble in a designed computer experiment. We develop quantitative and qualitative methods to compare observational data of the MOC with corresponding output from the ensemble, to learn about plausible input configurations of the model. Dimension reduction is used to express patterns of variation in model behaviour across the ensemble in a low-dimensional form. The ensemble is used to train an emulator; a fast statistical approximation to the expensive model, that includes an estimate of uncertainty due to the limited size of the ensemble. By training the emulator using the low-dimensional representations of the output, we are able to predict high-dimensional model output at input configurations not tested in the original ensemble. This allows a more complete expression of the uncertainty in the evolution of the MOC throughout the 21st century.
format Thesis
author McNeall, Douglas James
spellingShingle McNeall, Douglas James
Dimension reduction in the Bayesian analysis of a numerical climate model
author_facet McNeall, Douglas James
author_sort McNeall, Douglas James
title Dimension reduction in the Bayesian analysis of a numerical climate model
title_short Dimension reduction in the Bayesian analysis of a numerical climate model
title_full Dimension reduction in the Bayesian analysis of a numerical climate model
title_fullStr Dimension reduction in the Bayesian analysis of a numerical climate model
title_full_unstemmed Dimension reduction in the Bayesian analysis of a numerical climate model
title_sort dimension reduction in the bayesian analysis of a numerical climate model
publishDate 2008
url https://eprints.soton.ac.uk/69028/
https://eprints.soton.ac.uk/69028/1/McNeall_2008_PhD.pdf
genre North Atlantic
genre_facet North Atlantic
op_relation https://eprints.soton.ac.uk/69028/1/McNeall_2008_PhD.pdf
McNeall, Douglas James (2008) Dimension reduction in the Bayesian analysis of a numerical climate model. University of Southampton, Faculty of Engineering Science and Mathematics, School of Ocean and Earth Science, Doctoral Thesis, 176pp.
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