Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations

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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Published in:The Cryosphere
Main Authors: Felikson, Denis, Nowicki, Sophie, Nias, Isabel, Csatho, Beata, Schenk, Anton, Croteau, Michael J., Loomis, Bryant
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-4661-2023
https://tc.copernicus.org/articles/17/4661/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc107608 2024-09-15T18:09:26+00:00 Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations Felikson, Denis Nowicki, Sophie Nias, Isabel Csatho, Beata Schenk, Anton Croteau, Michael J. Loomis, Bryant 2023-11-07 application/pdf https://doi.org/10.5194/tc-17-4661-2023 https://tc.copernicus.org/articles/17/4661/2023/ eng eng doi:10.5194/tc-17-4661-2023 https://tc.copernicus.org/articles/17/4661/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-4661-2023 2024-08-28T05:24:15Z 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 The Cryosphere 17 11 4661 4673
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 J.
Loomis, Bryant
spellingShingle Felikson, Denis
Nowicki, Sophie
Nias, Isabel
Csatho, Beata
Schenk, Anton
Croteau, Michael J.
Loomis, Bryant
Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations
author_facet Felikson, Denis
Nowicki, Sophie
Nias, Isabel
Csatho, Beata
Schenk, Anton
Croteau, Michael J.
Loomis, Bryant
author_sort Felikson, Denis
title Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations
title_short Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations
title_full Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations
title_fullStr Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations
title_full_unstemmed Choice of observation type affects Bayesian calibration of Greenland Ice Sheet model simulations
title_sort choice of observation type affects bayesian calibration of greenland ice sheet model simulations
publishDate 2023
url https://doi.org/10.5194/tc-17-4661-2023
https://tc.copernicus.org/articles/17/4661/2023/
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-4661-2023
https://tc.copernicus.org/articles/17/4661/2023/
op_doi https://doi.org/10.5194/tc-17-4661-2023
container_title The Cryosphere
container_volume 17
container_issue 11
container_start_page 4661
op_container_end_page 4673
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