Greenland ice sheet runoff reduced by meltwater refreezing in bare ice
This paper reveals that current climate models overestimate Greenland Ice Sheet meltwater runoff because they don't account for significant refreezing within bare glacier ice. Field measurements and numerical modeling show that this refreezing reduces runoff by an estimated 11-17 Gt annually in southwest Greenland, suggesting an overlooked buffer against sea-level rise from ice melt.