333 results on '"GUDMUNDSSON, G. Hilmar"'
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2. Recent irreversible retreat phase of Pine Island Glacier
3. Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2)
4. Coupling framework (1.0) for the Úa (2023b) ice sheet model and the FESOM-1.4 z-coordinate ocean model in an Antarctic domain
5. Melt sensitivity of irreversible retreat of Pine Island Glacier
6. High spatial and temporal variability in Antarctic ice discharge linked to ice shelf buttressing and bed geometry
7. Sensitivity to forecast surface mass balance outweighs sensitivity to basal sliding descriptions for 21st century mass loss from three major Greenland outlet glaciers.
8. Weak relationship between remotely detected crevasses and inferred ice rheological parameters on Antarctic ice shelves.
9. Recent irreversible retreat phase of Pine Island Glacier
10. How accurate are estimates of glacier ice thickness? Results from ITMIX, the Ice Thickness Models Intercomparison eXperiment
11. Coupling framework (1.0) for the Úa (2023b) ice sheet model and the FESOM-1.4 z-coordinate ocean model in an Antarctic domain.
12. Melt sensitivity of irreversible retreat of Pine Island Glacier.
13. Experimental design for three interrelated marine ice sheet and ocean model intercomparison projects: MISMIP v. 3 (MISMIP+), ISOMIP v. 2 (ISOMIP+) and MISOMIP v. 1 (MISOMIP1)
14. Numerical stabilization methods for level-set-based ice front migration
15. The speedup of Pine Island Ice Shelf between 2017 and 2020: revaluating the importance of ice damage
16. Uncertainties in forecast surface mass balance outweigh uncertainties in basal sliding descriptions for 21st Century mass loss from three major Greenland outlet glaciers
17. Supplementary material to "Uncertainties in forecast surface mass balance outweigh uncertainties in basal sliding descriptions for 21st Century mass loss from three major Greenland outlet glaciers"
18. The stability of present-day Antarctic grounding lines – Part 2: Onset of irreversible retreat of Amundsen Sea glaciers under current climate on centennial timescales cannot be excluded
19. The stability of present-day Antarctic grounding lines – Part 1: No indication of marine ice sheet instability in the current geometry
20. Accurate coastal DEM generation by merging ASTER GDEM and ICESat/GLAS data over Mertz Glacier, Antarctica
21. Grounding-line migration in plan-view marine ice-sheet models: results of the ice2sea MISMIP3d intercomparison
22. In the Quest of a Parametric Relation Between Ice Sheet Model Inferred Weertman's Sliding‐Law Parameter and Airborne Radar‐Derived Basal Reflectivity Underneath Thwaites Glacier, Antarctica
23. Decadal Ocean Forcing and Antarctic Ice Sheet Response : LESSONS FROM THE AMUNDSEN SEA
24. Impact of marine processes on flow dynamics of northern Antarctic Peninsula outlet glaciers
25. Weak relationship between remotely detected crevasses and inferred ice rheological parameters on Antarctic ice shelves.
26. Numerical stabilization methods for level-set-based ice front migration.
27. Uncertainties in forecast surface mass balance outweigh uncertainties in basal sliding descriptions for 21st Century mass loss from three major Greenland outlet glaciers.
28. How calving could affect the future of Thwaites and Pine Island Glaciers
29. Has the (West) Antarctic Ice Sheet already tipped?
30. The Future of Thwaites Glacier, West Antarctica.
31. Predicting ocean-induced ice-shelf melt rates using deep learning
32. Incorporating Horizontal Density Variations into Large‐scale Modelling of Ice Masses
33. Recent irreversible retreat of Pine Island Glacier
34. The predictive power of ice sheet models and the regional sensitivity of ice loss to basal sliding parameterisations: a case study of Pine Island and Thwaites glaciers, West Antarctica
35. Inverse Methods in Glaciology
36. Slowdown of Shirase Glacier caused by strengthening alongshore winds
37. Supplementary material to "Slowdown of Shirase Glacier caused by strengthening alongshore winds"
38. Supplementary material to "The stability of present-day Antarctic grounding lines – Part A: No indication of marine ice sheet instability in the current geometry"
39. The stability of present-day Antarctic grounding lines – Part A: No indication of marine ice sheet instability in the current geometry
40. The predictive power of ice sheet models and the regional sensitivity of ice loss to basal sliding parameterisations: A case study of Pine Island and Thwaites Glaciers, West Antarctica
41. Increased warm water intrusions could cause mass loss in East Antarctica within 200 years
42. On the validity of the stress-flow angle as a metric for ice-shelf stability
43. Reversibility experiments of present-day Antarctic grounding lines: the long-term perspective
44. Reversibility experiments of present-day Antarctic grounding lines: the short-term perspective
45. The response of the Larsen C Ice Shelf to changes in ice-shelf buttressing
46. Reversibility experiments of present-day Antarctic grounding lines
47. Implementation of calving processes in large-scale ice sheet models
48. The instantaneous impact of calving and thinning on the Larsen C Ice Shelf
49. Slowdown of Shirase Glacier, East Antarctica, caused by strengthening alongshore winds.
50. Thermally induced temporal strain variations in rock walls observed at subzero temperatures
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