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Blink and You'll Miss It: An Investigation into Surging on Flade Isblink, Greenland 10.17863/CAM.9069 Cook, Samuel James Christoffersen, Poul Mass loss from fringing ice caps and glaciers in Greenland accounted for 20% of the ice sheet’s mass loss between 2003 and 2008 and could be responsible for up to 11 mm of sea- level rise by the end of the century. This study therefore applies a 3D, full-Stokes glaciological flow model, Elmer/Ice, to Flade Isblink, the largest fringing ice cap in Greenland, to investigate its basal conditions and the mechanism of a surge of two of its major outlet glaciers observed around the turn of the millennium. The results show that the ice cap is largely cold-based outside areas of fast flow, but that freezing also dominates in sliding areas. This implies an additional hydrological or heat input to allow the persistence of fast flow, the most likely candidate being surface meltwater and the associated latent heat release, leading to cryo-hydrologic warming. Model results indicate that the surge mechanism is a soft-bed thermal surge assisted by a hydro-thermodynamic feedback, with an estimated return period of 20-43 years. A till layer of 0.2-0.35 m thickness is inferred beneath sliding areas according to the hydrological budgets estimated for the surging glaciers. Results also indicate that this type of surge can self-terminate even without thinning of overlying ice, as slowdown will naturally reduce the frictional heat flux at the bed and thereby increase the release of latent heat of fusion due to basal freezing. Faster basal freezing will, in turn, produce a stronger bed and even slower ice flow due to withdrawal of pore water from the underlying till layer, which acts as a reservoir of latent heat as well as water. On the basis of these results, it is hypothesised that surging on Flade Isblink will increase in frequency over the coming decades, as more heat and meltwater will be stored in the subglacial till layer under global warming. University of Cambridge 2016-09-01 Thesis Masters Master of Philosophy (MPhil) en MPhil part-funded by the Newton Trust https://www.repository.cam.ac.uk/handle/1810/263707 https://apollo8-f-pro.lib.cam.ac.uk/bitstreams/24af692c-ca6b-45a0-9bc6-bd33234049e1/download 87eda9de84448d1f82354d60eee3eb5f https://apollo8-f-pro.lib.cam.ac.uk/bitstreams/d25f2eab-2132-4647-a54d-c0d39501eff5/download b462c5b61dbdb034a27c35accfd31004 https://apollo8-f-pro.lib.cam.ac.uk/bitstreams/f957f0e4-5261-4d5f-90c2-33b552a29640/download 5a20787812763526d20ddc5ca66ded86 https://www.rioxx.net/licenses/all-rights-reserved/ Glacier Surging Greenland Flade Isblink Ice Cap Ice Sheet Dynamics