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- W4256595816 abstract "Increased ablation under a greenhouse-effect climate is calculated by an energy-balance model for two sites at the margin of the Greenland ice sheet: Nordbogletscher, south Greenland, and Qamanârssûp sermia, West Greenland. The change in summer ablation is nearly linear with change in summer temperature, with gradients of 0.43 and 0.57 m water a −1 deg −1 for Nordbogletscher and Qamanârssûp sermia, respectively. However, the increase in ablation rate must be less in the higher parts of the ice sheet. A future climatic warming will therefore cause a rapid retreat of the ice-sheet margin and a steeper ice-sheet profile." @default.
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- W4256595816 date "1990-01-01" @default.
- W4256595816 modified "2023-10-16" @default.
- W4256595816 title "Increased Ablation at the Margin of the Greenland Ice Sheet under a Greenhouse-Effect Climate" @default.
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- W4256595816 doi "https://doi.org/10.3189/s0260305500008181" @default.
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