Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change

Abstract Mass loss from the Amundsen Sea Embayment of the West Antarctic Ice Sheet is a major contributor to global sea-level rise (SLR) and has been increasing over recent decades. Predictions of future SLR are increasingly modelled using ensembles of simulations within which model parameters and e...

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Published in:Journal of Glaciology
Main Authors: Bevan, Suzanne, Cornford, Stephen, Gilbert, Lin, Otosaka, Inés, Martin, Daniel, Surawy-Stepney, Trystan
Other Authors: Horizon 2020 Framework Programme
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2023.57
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000576
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spelling crcambridgeupr:10.1017/jog.2023.57 2024-03-03T08:36:36+00:00 Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change Bevan, Suzanne Cornford, Stephen Gilbert, Lin Otosaka, Inés Martin, Daniel Surawy-Stepney, Trystan Horizon 2020 Framework Programme 2023 http://dx.doi.org/10.1017/jog.2023.57 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000576 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology page 1-11 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2023.57 2024-02-08T08:29:18Z Abstract Mass loss from the Amundsen Sea Embayment of the West Antarctic Ice Sheet is a major contributor to global sea-level rise (SLR) and has been increasing over recent decades. Predictions of future SLR are increasingly modelled using ensembles of simulations within which model parameters and external forcings are varied within credible ranges. Accurately reporting the uncertainty associated with these predictions is crucial in enabling effective planning for, and construction of defences against, rising sea levels. Calibrating model simulations against current observations of ice-sheet behaviour enables the uncertainty to be reduced. Here we calibrate an ensemble of BISICLES ice-sheet model simulations of ice loss from the Amundsen Sea Embayment using remotely sensed observations of surface elevation and ice speed. Each calibration type is shown to be capable of reducing the 90% credibility bounds of predicted contributions to SLR by 34 and 43% respectively. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Ice Sheet Journal of Glaciology Cambridge University Press Antarctic Amundsen Sea West Antarctic Ice Sheet Journal of Glaciology 1 11
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Bevan, Suzanne
Cornford, Stephen
Gilbert, Lin
Otosaka, Inés
Martin, Daniel
Surawy-Stepney, Trystan
Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
topic_facet Earth-Surface Processes
description Abstract Mass loss from the Amundsen Sea Embayment of the West Antarctic Ice Sheet is a major contributor to global sea-level rise (SLR) and has been increasing over recent decades. Predictions of future SLR are increasingly modelled using ensembles of simulations within which model parameters and external forcings are varied within credible ranges. Accurately reporting the uncertainty associated with these predictions is crucial in enabling effective planning for, and construction of defences against, rising sea levels. Calibrating model simulations against current observations of ice-sheet behaviour enables the uncertainty to be reduced. Here we calibrate an ensemble of BISICLES ice-sheet model simulations of ice loss from the Amundsen Sea Embayment using remotely sensed observations of surface elevation and ice speed. Each calibration type is shown to be capable of reducing the 90% credibility bounds of predicted contributions to SLR by 34 and 43% respectively.
author2 Horizon 2020 Framework Programme
format Article in Journal/Newspaper
author Bevan, Suzanne
Cornford, Stephen
Gilbert, Lin
Otosaka, Inés
Martin, Daniel
Surawy-Stepney, Trystan
author_facet Bevan, Suzanne
Cornford, Stephen
Gilbert, Lin
Otosaka, Inés
Martin, Daniel
Surawy-Stepney, Trystan
author_sort Bevan, Suzanne
title Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
title_short Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
title_full Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
title_fullStr Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
title_full_unstemmed Amundsen Sea Embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
title_sort amundsen sea embayment ice-sheet mass-loss predictions to 2050 calibrated using observations of velocity and elevation change
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2023.57
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000576
geographic Antarctic
Amundsen Sea
West Antarctic Ice Sheet
geographic_facet Antarctic
Amundsen Sea
West Antarctic Ice Sheet
genre Amundsen Sea
Antarc*
Antarctic
Ice Sheet
Journal of Glaciology
genre_facet Amundsen Sea
Antarc*
Antarctic
Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
page 1-11
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2023.57
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 11
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