ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model

The contribution of the Antarctic ice sheet is one of the most uncertain components of sea level rise to 2100. Ice sheet models are the primary tool for projecting future sea level contribution from continental ice sheets. The Ice Sheet Model Intercomparison for the Coupled Model Intercomparison Pha...

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Main Authors: O'Neill, James F., Edwards, Tamsin L., Martin, Daniel F., Shafer, Courtney, Cornford, Stephen L., Seroussi, Helene L., Nowicki, Sophie, Adhikari, Mira
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-441
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-441/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere118162 2024-09-15T17:44:25+00:00 ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model O'Neill, James F. Edwards, Tamsin L. Martin, Daniel F. Shafer, Courtney Cornford, Stephen L. Seroussi, Helene L. Nowicki, Sophie Adhikari, Mira 2024-02-27 application/pdf https://doi.org/10.5194/egusphere-2024-441 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-441/ eng eng doi:10.5194/egusphere-2024-441 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-441/ eISSN: Text 2024 ftcopernicus https://doi.org/10.5194/egusphere-2024-441 2024-08-28T05:24:15Z The contribution of the Antarctic ice sheet is one of the most uncertain components of sea level rise to 2100. Ice sheet models are the primary tool for projecting future sea level contribution from continental ice sheets. The Ice Sheet Model Intercomparison for the Coupled Model Intercomparison Phase 6 (ISMIP6) provided projections of the ice sheets contribution to sea level over the 21st century. It quantified uncertainty due to ice sheet model, climate scenario, forcing climate model and uncertain model parameters. We present simulations following the ISMIP6 framework with the BISICLES ice sheet model, alongside new experiments extending the ISMIP6 protocol to more comprehensively explore uncertain ice sheet processes. These results contributed to Antarctic projections of Edwards et al. (2021), which formed the basis of sea level projections for the Sixth Assessment Report of the Intergovernmental Panel on Climate Change (AR6). The BISICLES experiments presented here show the important interplay between surface mass balance forcing and ocean driven melt, with high warming, high accumulation forcing conditions leading to mass gain (negative sea level contribution) under low sensitivity to ocean driven melt. Conversely, we show that when sensitivity to ocean warming is high, ocean melting drives increased mass loss despite high accumulation. Finally, we show that collapse of ice shelves due to surface warming increases sea level contribution by 25 mm for both moderate and high sensitivity of ice shelf melting to ocean forcing tested. Text Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The contribution of the Antarctic ice sheet is one of the most uncertain components of sea level rise to 2100. Ice sheet models are the primary tool for projecting future sea level contribution from continental ice sheets. The Ice Sheet Model Intercomparison for the Coupled Model Intercomparison Phase 6 (ISMIP6) provided projections of the ice sheets contribution to sea level over the 21st century. It quantified uncertainty due to ice sheet model, climate scenario, forcing climate model and uncertain model parameters. We present simulations following the ISMIP6 framework with the BISICLES ice sheet model, alongside new experiments extending the ISMIP6 protocol to more comprehensively explore uncertain ice sheet processes. These results contributed to Antarctic projections of Edwards et al. (2021), which formed the basis of sea level projections for the Sixth Assessment Report of the Intergovernmental Panel on Climate Change (AR6). The BISICLES experiments presented here show the important interplay between surface mass balance forcing and ocean driven melt, with high warming, high accumulation forcing conditions leading to mass gain (negative sea level contribution) under low sensitivity to ocean driven melt. Conversely, we show that when sensitivity to ocean warming is high, ocean melting drives increased mass loss despite high accumulation. Finally, we show that collapse of ice shelves due to surface warming increases sea level contribution by 25 mm for both moderate and high sensitivity of ice shelf melting to ocean forcing tested.
format Text
author O'Neill, James F.
Edwards, Tamsin L.
Martin, Daniel F.
Shafer, Courtney
Cornford, Stephen L.
Seroussi, Helene L.
Nowicki, Sophie
Adhikari, Mira
spellingShingle O'Neill, James F.
Edwards, Tamsin L.
Martin, Daniel F.
Shafer, Courtney
Cornford, Stephen L.
Seroussi, Helene L.
Nowicki, Sophie
Adhikari, Mira
ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model
author_facet O'Neill, James F.
Edwards, Tamsin L.
Martin, Daniel F.
Shafer, Courtney
Cornford, Stephen L.
Seroussi, Helene L.
Nowicki, Sophie
Adhikari, Mira
author_sort O'Neill, James F.
title ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model
title_short ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model
title_full ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model
title_fullStr ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model
title_full_unstemmed ISMIP6-based Antarctic Projections to 2100: simulations with the BISICLES ice sheet model
title_sort ismip6-based antarctic projections to 2100: simulations with the bisicles ice sheet model
publishDate 2024
url https://doi.org/10.5194/egusphere-2024-441
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-441/
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
op_source eISSN:
op_relation doi:10.5194/egusphere-2024-441
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-441/
op_doi https://doi.org/10.5194/egusphere-2024-441
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