Concurrent superimposed ice formation and meltwater runoff on Greenland’s ice slabs

Rivers and slush fields on the Greenland Ice Sheet increasingly develop in locations where the accumulation zone hosts near-impermeable ice slabs. However, the division between runoff versus retention in these areas remains unmeasured. We present field measurements of superimposed ice formation onto slabs around the visible runoff limit. The quantity of superimposed ice varies by proximity to visible surface water and the surface slope, highlighting that meltwater can flow laterally before refreezing. We use heat conduction modelling and radar observations of autumn wetness to show that in our field area in 2022, 65% of superimposed ice formed during summer and the rest during autumn in the relict supraglacial hydrological network. Overall, 84% of melt around the visible runoff limit refroze. Ice-sheet-wide we estimate that slabs refroze 56 gigatonnes of melt (26-69 gigatonnes according to slab extent) between 2017 and 2022. Slabs are thus both hotspots of refreezing and emerging zones of runoff.

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Publication Details

Journal
Nature Communications
Published
2025-05-14
DOI
https://doi.org/10.1038/s41467-025-59237-9
Citations
3
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
3.90

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article

Concurrent superimposed ice formation and meltwater runoff on Greenland’s ice slabs

Marco Tedesco, Stef Lhermitte, Dirk van As, Hannah Picton et al.
3 citations
Nature Communications
Cryospheric studies and observations
3.90
article

Concurrent superimposed ice formation and meltwater runoff on Greenland’s ice slabs

Marco Tedesco, Stef Lhermitte, Dirk van As, Hannah Picton, Andrew Tedstone, Horst Machguth, Paolo Colosio, Nicole Clerx, Nicolas Jullien, Julien Ducrey
article en
3 citations

Abstract

Rivers and slush fields on the Greenland Ice Sheet increasingly develop in locations where the accumulation zone hosts near-impermeable ice slabs. However, the division between runoff versus retention in these areas remains unmeasured. We present field measurements of superimposed ice formation onto slabs around the visible runoff limit. The quantity of superimposed ice varies by proximity to visible surface water and the surface slope, highlighting that meltwater can flow laterally before refreezing. We use heat conduction modelling and radar observations of autumn wetness to show that in our field area in 2022, 65% of superimposed ice formed during summer and the rest during autumn in the relict supraglacial hydrological network. Overall, 84% of melt around the visible runoff limit refroze. Ice-sheet-wide we estimate that slabs refroze 56 gigatonnes of melt (26-69 gigatonnes according to slab extent) between 2017 and 2022. Slabs are thus both hotspots of refreezing and emerging zones of runoff.

Nature CommunicationsVol. 16(1)
Lamont-Doherty Earth Observatory (US), University of Fribourg (CH), Geological Survey of Denmark and Greenland (DK), École Polytechnique Fédérale de Lausanne (CH), Columbia University (US), University of Brescia (IT), University of Lausanne (CH), Delft University of Technology (NL), University of Edinburgh (GB), KU Leuven (BE)
National Science Foundation, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Swiss Polar Institute, Natural Environment Research Council
Climate action
Openalex Percentile: Top 7%
Cryospheric studies and observations
3.90
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