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Unravelling the long-term, locally heterogenous response of Greenland glaciers o...
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Unravelling the long-term, locally heterogenous response of Greenland glaciers o...
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The role of meltwater in high-latitude trough-mouth fan development: The Disko T...
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Accelerating glacier mass loss on Franz Josef Land, Russian Arctic
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Intra- and inter-annual variability in dynamic discharge from the Academy of Sci...
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Flow of the West Antarctic Ice Sheet on the continental margin of the Bellingsha...
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Sediment‐rich meltwater plumes and ice‐proximal fans at the margins of modern an...
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Ice-stream stability on a reverse bed slope
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Is breaking up hard to do? Clues from the sea bed
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Past water flow beneath Pine Island and Thwaites glaciers, West Antarctica
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Past water flow beneath Pine Island and Thwaites glaciers, West Antarctica
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Past water flow beneath Pine Island and Thwaites glaciers, West Antarctica
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Ice-stream stability on a reverse bed slope
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Flow dynamics and till genesis associated with a marine-based Antarctic palaeo-i...
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Variability in ice motion and dynamic discharge from Devon Ice Cap, Nunavut, Can...
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THE NORWEGIAN–GREENLAND SEA CONTINENTAL MARGINS: MORPHOLOGY AND LATE QUATERNARY...
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Flow dynamics and till genesis associated with a marine-based Antarctic palaeo-i...
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Towards modelling of corrugation ridges at ice-sheet grounding lines
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Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day.
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Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day. ...
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