24 results on '"Alley, Richard B."'
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2. Multidecadal pre- and post-collapse dynamics of the northern Larsen Ice Shelf
3. Ice-Shelf Flexure and Tidal Forcing of Bindschadler Ice Stream, West Antarctica
4. Interpretation of topography and bed properties beneath Thwaites Glacier, West Antarctica using seismic reflection methods
5. Ice-Shelf Tidal Flexure and Subglacial Pressure Variations
6. Evaluation of ice-stream model sensitivities for parameter estimation
7. The impact of spatially-variable basal properties on outlet glacier flow
8. Relating bed character and subglacial morphology using seismic data from Thwaites Glacier, West Antarctica
9. Earth rotation changes since −500 CE driven by ice mass variations
10. Basal characteristics of the main sticky spot on the ice plain of Whillans Ice Stream, Antarctica
11. Subglacial bathymetry and sediment distribution beneath Pine Island Glacier ice shelf modeled using aerogravity and in situ geophysical data: New results
12. Glacier velocity variability due to rain-induced sliding and cavity formation
13. Potential Antarctic Ice Sheet retreat driven by hydrofracturing and ice cliff failure
14. Dilatant till facilitates ice-stream flow in northeast Greenland
15. Holocene dynamics of the Rhone Glacier, Switzerland, deduced from ice flow models and cosmogenic nuclides
16. Subglacial Lake Whillans — Ice-penetrating radar and GPS observations of a shallow active reservoir beneath a West Antarctic ice stream
17. Subglacial Lake Whillans — Seismic observations of a shallow active reservoir beneath a West Antarctic ice stream
18. A viscoelastic flowline model applied to tidal forcing of Bindschadler Ice Stream, West Antarctica
19. Dynamics of stick–slip motion, Whillans Ice Stream, Antarctica
20. On the nature of the dirty ice at the bottom of the GISP2 ice core
21. Glacial advance and stagnation caused by rock avalanches
22. Initial effects of oceanic warming on a coupled ocean–ice shelf–ice stream system
23. Reply to Shulmeister et al. comment on “Glacial advance and stagnation caused by Rock Avalanches”
24. Rapid response of modern day ice sheets to external forcing
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