Diverging runoff drives uncertainty in Antarctic surface mass balance projections under a high emission scenario

Abstract. Three recent downscalings of CESM with MAR, RACMO, and HIRHAM under SSP5-8.5 produce consistent contemporary Antarctic surface mass balance (SMB), but diverge strongly by 2100, especially over ice shelves. HIRHAM simulates a large SMB decline driven by strong runoff increases, MAR a moderate decrease, while RACMO maintains near balance. These differences mainly reflect contrasting melt–albedo feedbacks, present-day melt and refreezing levels, and a persistent 1–2 °C temperature offset between MAR and RACMO. CESM shows a decline similar in magnitude to MAR, with high melt partly compensated by extensive refreezing. Over grounded ice, all models project increased SMB from higher snowfall, though runoff still drives their spread. Despite shared boundary conditions and similar contemporary SMB, model behavior diverges, and CESM’s integrated results resemble MAR's despite its coarse resolution. Performance differences in present-day melt suggest that uncertainty estimates should account for model skill, motivating Bayesian treatment of multi-model ensembles.

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Publication Details

Journal
The Cryosphere
Published
2026-11-09
DOI
https://doi.org/10.5194/tc-20-6353-2026
Citations
1
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
1.66

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article

Diverging runoff drives uncertainty in Antarctic surface mass balance projections under a high emission scenario

M. R. van den Broeke, René R. Wijngaard, Gaël Durand, Quentin Glaude et al.
1 citations
The Cryosphere
Cryospheric studies and observations
1.66
article

Diverging runoff drives uncertainty in Antarctic surface mass balance projections under a high emission scenario

M. R. van den Broeke, René R. Wijngaard, Gaël Durand, Quentin Glaude, Christoph Kittel, Vincent Favier, Heiko Goelzer, Xavier Fettweis, Martin Olesen, Ruth H. Mottram, Fredrik Boberg, Willem Jan van de Berg, Nicolaj Hansen, Nicolas C. Jourdain, Charles Amory, Benjamin Heurgue
article en
1 citations

Abstract

Abstract. Three recent downscalings of CESM with MAR, RACMO, and HIRHAM under SSP5-8.5 produce consistent contemporary Antarctic surface mass balance (SMB), but diverge strongly by 2100, especially over ice shelves. HIRHAM simulates a large SMB decline driven by strong runoff increases, MAR a moderate decrease, while RACMO maintains near balance. These differences mainly reflect contrasting melt–albedo feedbacks, present-day melt and refreezing levels, and a persistent 1–2 °C temperature offset between MAR and RACMO. CESM shows a decline similar in magnitude to MAR, with high melt partly compensated by extensive refreezing. Over grounded ice, all models project increased SMB from higher snowfall, though runoff still drives their spread. Despite shared boundary conditions and similar contemporary SMB, model behavior diverges, and CESM’s integrated results resemble MAR's despite its coarse resolution. Performance differences in present-day melt suggest that uncertainty estimates should account for model skill, motivating Bayesian treatment of multi-model ensembles.

The CryosphereVol. 20(11)
Centre National de la Recherche Scientifique (FR), Vrije Universiteit Brussel (BE), University of Liège (BE), Utrecht University (NL), Bjerknes Centre for Climate Research (NO), Danish Meteorological Institute (DK), NORCE Research AS (NO), Institut des Géosciences de l'Environnement (FR), Institut de Recherche pour le Développement (FR)
European Commission, Agence Nationale de la Recherche, Fonds De La Recherche Scientifique - FNRS, Novo Nordisk, Novo Nordisk Fonden, Horizon 2020
Climate action
Openalex Percentile: Top 27%
Cryospheric studies and observations
1.66
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