PALAEO-ICE STREAMS IN THE NORTH-EASTERN LAURENTIDE ICE SHEET
, 2007 This thesis presents a palaeoglaciological study aimed to determine the location, geometry and temporal evolution of palaeo-ice streams of the north-easternmost Laurentide Ice Sheet. The work was accomplished through the geomorphological interpretation of satellite imagery over 3.19 x 106 km2 of the Canadian Arctic, using a glaciological inversion ...
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Micro-earthquakes beneath Ice Streams Β and C, West Antarctica: observations and implications [PDF]
, 1993 S. Anandakrishnan, C. R. Bentley
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Genese des Nordseeraumes im Quartär
Fennia: International Journal of Geography, 1974 In spite of alterations due to transgressions, Pleistocene forms are still discernible in the North Sea area. In this study, explanation of their genesis is based on a reconstruction of the ice‑sheds of different dimensions and the dynamic elements of ...
Heinrich Reinhard
doaj
Studies of the grounding-line location on Ice Streams D and E, Antarctica [PDF]
, 1994 R. W. Jacobel +2 more
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Evaluation of strain rates on Ice Stream B, Antarctica, obtained using GPS phase measurements [PDF]
, 1994 Christina Hulbe, I. M. Whillans
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Sustained ocean cooling insufficient to reverse sea level rise from Antarctica
Communications Earth & EnvironmentGlobal mean sea level has risen at an accelerating rate in the last decade and will continue to rise for centuries. The Amundsen Sea Embayment in West Antarctica is a critical region for present and future ice loss, however most studies consider only a ...
Alanna Alevropoulos-Borrill +4 more
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The origin and longevity of flow stripes on Antarctic ice streams [PDF]
, 1998 G. Hilmar Gudmundsson +2 more
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Ice-Shelf Tidal Flexure and Subglacial Pressure Variations [PDF]
We develop a model of an ice shelf-ice stream system as a viscoelastic beam partially supported by an elastic foundation. When bed rock near the grounding line acts as a fulcrum, leverage from the ice shelf dropping at low tide can cause significant ...
Alley, Richard B. +5 more
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Surface velocity and mass balance of Ice Streams D and E, West Antarctica [PDF]
, 1996 Robert Bindschadler +4 more
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Radar reflections reveal a wet bed beneath stagnant Ice Stream C and a frozen bed beneath ridge BC, West Antarctica [PDF]
, 1998 Charles R. Bentley +2 more
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