Modeled Greenland Ice Sheet evolution constrained by ice-core-derived Holocene elevation histories

During the Holocene, the Greenland Ice Sheet (GrIS) experienced substantial thinning, with some regions losing up to 600 meters of ice. Ice sheet reconstructions, paleoclimatic records, and geological evidence indicate that during the Last Glacial Maximum, the GrIS extended far beyond its current bo...

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Bibliographic Details
Main Authors: Lauritzen, Mikkel Langgaard, Solgaard, Anne Munck, Rathmann, Nicholas Mossor, Vinther, Bo Møllesøe, Grindsted, Aslak, Noël, Brice, Aðalgeirsdóttir, Guðfinna, Hvidberg, Christine Schøtt
Format: Text
Language:English
Published: 2024
Subjects:
Greenland
ice core
Ice Sheet
Online Access:https://doi.org/10.5194/egusphere-2024-2223
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2223/
Description
Summary:During the Holocene, the Greenland Ice Sheet (GrIS) experienced substantial thinning, with some regions losing up to 600 meters of ice. Ice sheet reconstructions, paleoclimatic records, and geological evidence indicate that during the Last Glacial Maximum, the GrIS extended far beyond its current boundaries and was connected with the Innuitian Ice Sheet (IIS) in the northwest. We investigate these long-term geometry changes and explore several possible factors driving those changes by using the Parallel Ice Sheet Model (PISM) to simulate the GrIS thinning throughout the Holocene period, from 11.7 ka ago to the present. We perform an ensemble study of 841 model simulations in which key model parameters are systematically varied to determine the parameter values that, with quantified uncertainties, best reproduce the 11.7 ka of surface elevation records derived from ice cores, providing confidence in the modeled GrIS historical evolution. We find that since the Holocene onset, 11.7 ka ago, the GrIS mass loss has contributed 5.3±0.3 m to the mean global sea level rise, which is consistent with the ice-core-derived thinning curves spanning the time when the GrIS and the Innuitian Ice Sheet were bridged. Our results suggest that the ice bridge collapsed 4.9±0.5 ka ago and that the GrIS is still responding to these past changes today, having raised sea level by 23±26 mm SLE ka -1 in the last 500 years. Our results have implications for future mass-loss projections, which should account for this long-term, transient trend.

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