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Supraglacial lakes on the Greenland ice sheet advance inland under warming climate


Supraglacial lakes (SGLs) form annually on the Greenland ice sheet1,2 and, when they drain, their discharge enhances ice-sheet flow3 by lubricating the base4 and potentially by warming the ice5. Today, SGLs tend to form within the ablation zone, where enhanced lubrication is offset by efficient subglacial drainage6,7. However, it is not clear what impact a warming climate will have on this arrangement. Here, we use an SGL initiation and growth8 model to show that lakes form at higher altitudes as temperatures rise, consistent with satellite observations9. Our simulations show that in southwest Greenland, SGLs spread 103 and 110 km further inland by the year 2060 under moderate (RCP 4.5) and extreme (RCP 8.5) climate change scenarios, respectively, leading to an estimated 48–53% increase in the area over which they are distributed across the ice sheet as a whole. Up to half of these new lakes may be large enough to drain, potentially delivering water and heat to the ice-sheet base in regions where subglacial drainage is inefficient. In such places, ice flow responds positively to increases in surface water delivered to the bed through enhanced basal lubrication4,10,11 and warming of the ice5, and so the inland advance of SGLs should be considered in projections of ice-sheet change.

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Figure 1: Simulated distribution of SGLs in 2050–2060 under projections of climate change.
Figure 2: Simulated and observed trends in maximum lake elevation.
Figure 3: Future inland migration of SGLs on the Greenland ice sheet.


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This work was supported by the UK National Centre for Earth Observation. We also acknowledge M. van den Broeke who supplied surface mass balance estimates produced using the RACMO model to I.H.

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Authors and Affiliations



A.A.L. and A.S. designed the research. A.A.L. wrote and developed the SLInG model and performed all simulations/analysis. K.B. and A.A.L. created the surface DEM used as input into the SLInG model. X.F. provided runoff data from MAR simulations. M.M. and E.R. provided the bedrock DEM. I.H. provided satellite observations and equilibrium line altitude estimates. A.A.L. and A.S. wrote the paper. All authors discussed the results and commented on the manuscript.

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Correspondence to A. A. Leeson.

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Leeson, A., Shepherd, A., Briggs, K. et al. Supraglacial lakes on the Greenland ice sheet advance inland under warming climate. Nature Clim Change 5, 51–55 (2015).

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