215 results on '"Vaughan, David G."'
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2. A Reconciled Estimate of Ice-Sheet Mass Balance
3. Recent Trends in Melting Conditions on the Antarctic Peninsula and Their Implications for Ice-Sheet Mass Balance and Sea Level
4. High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector
5. Supplementary material to "High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector"
6. High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector
7. British Antarctic Survey's aerogeophysical data: releasing 25 years of airborne gravity, magnetic, and radar datasets over Antarctica
8. Devil in the Detail
9. Widespread Complex Flow in the Interior of the Antarctic Ice Sheet
10. Supplementary material to "British Antarctic Survey’s Aerogeophysical Data: Releasing 25 Years of Airborne Gravity, Magnetic, and Radar Datasets over Antarctica"
11. Why Is It Hard to Predict the Future of Ice Sheets?
12. Multisystem Synthesis of Radar Sounding Observations of the Amundsen Sea Sector From the 2004–2005 Field Season
13. High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector.
14. Reassessment of Net Surface Mass Balance in Antarctica
15. Antarctic Snow Accumulation Mapped Using Polarization of 4.3-cm Wavelength Microwave Emission
16. New Boundary Conditions for the West Antarctic Ice Sheet: Subglacial Topography of the Thwaites and Smith Glacier Catchments
17. Summary for Policymakers
18. Inland thinning of West Antarctic Ice Sheet steered along subglacial rifts
19. Polar research: Six priorities for Antarctic science
20. Amundsen Sea bathymetry: the benefits of using gravity data for bathymetric prediction
21. Extensive dynamic thinning on the margins of the Greenland and Antarctic ice sheets
22. West Antarctic Ice Sheet collapse – the fall and rise of a paradigm
23. Spatial and Temporal Variation of Surface Temperature on the Antarctic Peninsula And The Limit of Viability of Ice Shelves
24. A Review of Pine Island Glacier, West Antarctica: Hypotheses of Instability Vs. Observations of Change
25. East Antarctic ice stream tributary underlain by major sedimentary basin
26. Diverse landscapes beneath Pine Island Glacier influence ice flow
27. Subglacial lakes and hydrology across the Ellsworth Subglacial Highlands, West Antarctica
28. Recent Rapid Regional Climate Warming on the Antarctic Peninsula
29. Risk Estimation of Collapse of the West Antarctic Ice Sheet
30. Ice Sheets
31. Contributors
32. Supplementary material to "Subglacial lakes and hydrology across the Ellsworth Subglacial Highlands, West Antarctica"
33. How Does the Antarctic Ice Sheet Affect Sea Level Rise?
34. Distortion of isochronous layers in ice revealed by ground-penetrating radar
35. Variability of Basal Melt Beneath the Pine Island Glacier Ice Shelf, West Antarctica
36. Sustained Antarctic Research: A 21st Century Imperative
37. Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry
38. Supplementary material to "Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry"
39. Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry
40. Geothermal Heat Flux Reveals the Iceland Hotspot Track Underneath Greenland
41. How dynamic are ice-stream beds?
42. Heat Flux Distribution of Antarctica Unveiled
43. How dynamic are ice-stream beds?
44. Observations: Cryosphere
45. Sea-bed corrugations beneath an Antarctic ice shelf revealed by autonomous underwater vehicle survey: Origin and implications for the history of Pine Island Glacier
46. Sustained Antarctic Research: A 21stCentury Imperative
47. A ‘continuity-index’ for assessing ice-sheet dynamics from radar-sounded internal layers
48. Subglacial melt channels and fracture in the floating part of Pine Island Glacier, Antarctica
49. Multi-decadal glacier surface lowering in the Antarctic Peninsula
50. Investigating Greenland Ice Sheet dynamics using high resolution full-Stokes simulations
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