692 results on '"Alley, Richard B."'
Search Results
152. Subglacial Lake Whillans — Ice-penetrating radar and GPS observations of a shallow active reservoir beneath a West Antarctic ice stream
153. Subglacial Lake Whillans — Seismic observations of a shallow active reservoir beneath a West Antarctic ice stream
154. A viscoelastic flowline model applied to tidal forcing of Bindschadler Ice Stream, West Antarctica
155. Oceanic Forcing of Ice-Sheet Retreat: West Antarctica and More
156. Dynamic perennial firn aquifer on an Arctic glacier
157. Increasing temperature forcing reduces the Greenland Ice Sheet’s response time scale
158. Dynamics of stick–slip motion, Whillans Ice Stream, Antarctica
159. North Atlantic climate variability from a self-organizing map perspective
160. Summary for Policymakers
161. A Few Preliminary Results from the Glaciogeophysical Survey of the Interior Ross Embayment (GSIRE)
162. On thickening ice? (Perspectives: Climate Change)
163. On the nature of the dirty ice at the bottom of the GISP2 ice core
164. Glacial advance and stagnation caused by rock avalanches
165. Implications of abrupt climate change
166. Seismic and geodetic evidence for grounding-line control of Whillans Ice Stream stick-slip events
167. Physical properties of the WAIS Divide ice core
168. Basal conditions and ice dynamics inferred from radar-derived internal stratigraphy of the northeast Greenland ice stream
169. Tidal pacing, skipped slips and the slowdown of Whillans Ice Stream, Antarctica
170. Tidally controlled stick-slip discharge of aWest Antarctic Ice
171. Ice sheet grounding zone stabilization due to till compaction
172. Initial effects of oceanic warming on a coupled ocean–ice shelf–ice stream system
173. Icing the North Atlantic
174. Sediment deposition at the modern grounding zone of Whillans Ice Stream, West Antarctica
175. Bathymetry and geological structures beneath the Ross Ice Shelf at the mouth of Whillans Ice Stream, West Antarctica, modeled from ground-based gravity measurements
176. Watchable Wildlife and Demand-Driven General Education
177. Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
178. Subglacial bathymetry and sediment layer distribution beneath the Pine Island Glacier ice shelf, West Antarctica, modeled using aerogravity and autonomous underwater vehicle data
179. Ice-Sheet Response to Oceanic Forcing
180. Reaching Out Beyond the Usual Suspects and Traditional Media: Re-branding Climate Change as a Problem with a Feasible Solution.
181. The role of channelized basal melt in ice-shelf stability: recent progress and future priorities.
182. Motion of an Antarctic glacier by repeated tidally modulated earthquakes
183. Seasonal to decadal scale variations in the surface velocity of Jakobshavn Isbrae, Greenland: Observation and model‐based analysis
184. Modeling Ice-Sheet Flow
185. Improved moraine age interpretations through explicit matching of geomorphic process models to cosmogenic nuclide measurements from single landforms
186. Greenland was nearly ice-free for extended periods during the Pleistocene
187. Stability of the West Antarctic ice sheet in a warming world
188. Exploring till bed kinematics using AMS magnetic fabrics and pebble fabrics: the Weedsport drumlin field, New York State, USA
189. Geological record of ice shelf break-up and grounding line retreat, Pine Island Bay, West Antarctica
190. The Rhone Glacier was smaller than today for most of the Holocene
191. Englacial seismic reflectivity: imaging crystal-orientation fabric in West Antarctica
192. Reply to Shulmeister et al. comment on “Glacial advance and stagnation caused by Rock Avalanches”
193. Past rates of climate change in the Arctic
194. History of sea ice in the Arctic
195. Arctic amplification: can the past constrain the future?
196. History of the Greenland Ice Sheet: paleoclimatic insights
197. Arctic Paleoclimate Synthesis Thematic Papers
198. Origin of stratified basal ice in outlet glaciers of Vatnajökull and Öræfajökull, Iceland
199. Putting the Younger Dryas cold event into context
200. Numerical modeling of valley glacier stagnation as a paleoclimatic indicator
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