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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Bibliographic Details
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:
Antarctic
The Antarctic
Antarc*
Ice Sheet
Ice Shelf
Ice Shelves
Online Access:https://doi.org/10.5194/egusphere-2024-441
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-441/
Description
Summary: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.

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