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Rapid increases in satellite-observed ice sheet surface meltwater production
Zheng, L.; Shang, X.; van den Broeke, M.R.; Noël, B.; Li, X.; Fettweis, X.; Liang, Q.; Wang, K.; Liu, J.; Cheng, X. (2025). Rapid increases in satellite-observed ice sheet surface meltwater production. Nat. Clim. Chang. 15(7): 769-774. https://dx.doi.org/10.1038/s41558-025-02364-4
In: Nature Climate Change. Nature Publishing Group: London. ISSN 1758-678X; e-ISSN 1758-6798, more
Related to:
Boghosian, A.L. (2025). East Antarctica slides into the spotlight as surface melt hotspot. Nat. Clim. Chang. 15(7): 694-695. https://dx.doi.org/10.1038/s41558-025-02371-5, more
Peer reviewed article  

Available in  Authors 

Authors  Top 
  • Zheng, L.
  • Shang, X.
  • van den Broeke, M.R.
  • Noël, B., more
  • Li, X.
  • Fettweis, X., more
  • Liang, Q.
  • Wang, K.
  • Liu, J.
  • Cheng, X.

Abstract
    Surface meltwater production influences the contribution of ice sheets to global sea-level change. Ice-sheet-wide meltwater production has thus far primarily been quantified by regional climate models. Here we present a 31-year (1992–2023) time series of daily satellite-observed surface melt flux for the Greenland and Antarctic ice sheets. The annual meltwater volume in Greenland has significantly increased, with intensified melt in the northern basins dominated by a negative North Atlantic Oscillation and elevated melt flux in western basins driven by the decline in Arctic sea-ice. In East Antarctica, high melt rates since 2000 are attributed to warm air incursions from the Southern Ocean due to anomalous atmospheric circulations associated with a negative Southern Annular Mode and the recovery of the Antarctic ozone hole. This region, previously less prone to surface melt, has become a melt hotspot, potentially leading to meltwater ponding and future ice shelf destabilization.

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