Choice of observation type affects Bayesian calibration of ice sheet model projections

Determining reliable probability distributions for ice sheet mass change over the coming century is critical to refining uncertainties in sea-level rise projections. Bayesian calibration, a method for constraining projection uncertainty using observations, has been previously applied to ice sheet pr...

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Main Authors: Felikson, Denis, Nowicki, Sophie, Nias, Isabel, Csatho, Beata, Schenk, Anton, Croteau, Michael, Loomis, Bryant
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-1213
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1213/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere107608 2023-12-10T09:49:10+01:00 Choice of observation type affects Bayesian calibration of ice sheet model projections Felikson, Denis Nowicki, Sophie Nias, Isabel Csatho, Beata Schenk, Anton Croteau, Michael Loomis, Bryant 2023-11-07 application/pdf https://doi.org/10.5194/egusphere-2022-1213 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1213/ eng eng doi:10.5194/egusphere-2022-1213 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1213/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2022-1213 2023-11-13T17:24:19Z Determining reliable probability distributions for ice sheet mass change over the coming century is critical to refining uncertainties in sea-level rise projections. Bayesian calibration, a method for constraining projection uncertainty using observations, has been previously applied to ice sheet projections but the impact of the chosen observation type on the calibrated posterior probability distributions has not been quantified. Here, we perform three separate Bayesian calibrations to constrain uncertainty in Greenland Ice Sheet (GrIS) simulations of the committed mass loss in 2100 under the current climate, using observations of velocity change, dynamic ice thickness change, and mass change. Comparing the posterior probability distributions shows that the median ice sheet mass change can differ by 119 % for the particular model ensemble that we used, depending on the observation type used in the calibration. More importantly for risk-averse sea-level planning, posterior probabilities of high-end mass change scenarios are highly sensitive to the observation selected for calibration. Furthermore, we show that using mass change observations alone may result in model simulations that overestimate flow acceleration and underestimate dynamic thinning around the margin of the ice sheet. Finally, we look ahead and present ideas for ways to improve Bayesian calibration of ice sheet projections. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Determining reliable probability distributions for ice sheet mass change over the coming century is critical to refining uncertainties in sea-level rise projections. Bayesian calibration, a method for constraining projection uncertainty using observations, has been previously applied to ice sheet projections but the impact of the chosen observation type on the calibrated posterior probability distributions has not been quantified. Here, we perform three separate Bayesian calibrations to constrain uncertainty in Greenland Ice Sheet (GrIS) simulations of the committed mass loss in 2100 under the current climate, using observations of velocity change, dynamic ice thickness change, and mass change. Comparing the posterior probability distributions shows that the median ice sheet mass change can differ by 119 % for the particular model ensemble that we used, depending on the observation type used in the calibration. More importantly for risk-averse sea-level planning, posterior probabilities of high-end mass change scenarios are highly sensitive to the observation selected for calibration. Furthermore, we show that using mass change observations alone may result in model simulations that overestimate flow acceleration and underestimate dynamic thinning around the margin of the ice sheet. Finally, we look ahead and present ideas for ways to improve Bayesian calibration of ice sheet projections.
format Text
author Felikson, Denis
Nowicki, Sophie
Nias, Isabel
Csatho, Beata
Schenk, Anton
Croteau, Michael
Loomis, Bryant
spellingShingle Felikson, Denis
Nowicki, Sophie
Nias, Isabel
Csatho, Beata
Schenk, Anton
Croteau, Michael
Loomis, Bryant
Choice of observation type affects Bayesian calibration of ice sheet model projections
author_facet Felikson, Denis
Nowicki, Sophie
Nias, Isabel
Csatho, Beata
Schenk, Anton
Croteau, Michael
Loomis, Bryant
author_sort Felikson, Denis
title Choice of observation type affects Bayesian calibration of ice sheet model projections
title_short Choice of observation type affects Bayesian calibration of ice sheet model projections
title_full Choice of observation type affects Bayesian calibration of ice sheet model projections
title_fullStr Choice of observation type affects Bayesian calibration of ice sheet model projections
title_full_unstemmed Choice of observation type affects Bayesian calibration of ice sheet model projections
title_sort choice of observation type affects bayesian calibration of ice sheet model projections
publishDate 2023
url https://doi.org/10.5194/egusphere-2022-1213
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1213/
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source eISSN:
op_relation doi:10.5194/egusphere-2022-1213
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1213/
op_doi https://doi.org/10.5194/egusphere-2022-1213
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