Results 21 to 30 of about 200,024 (256)

Of isbræ and ice streams [PDF]

open access: yesAnnals of Glaciology, 2003
AbstractFast-flowing ice streams and outlet glaciers provide the major avenues for ice flow from past and present ice sheets. These ice streams move faster than the surrounding ice sheet by a factor of 100 or more. Several mechanisms for fast ice-stream flow have been identified, leading to a spectrum of different ice-stream types.
Martin Truffer, Keith A. Echelmeyer
openaire   +2 more sources

Palaeo-ice streams: an introduction [PDF]

open access: yesBoreas, 2003
[FIRST PARAGRAPH] Ice streams are narrow fast-flowing zones within ice sheets, and in the case of Antarctica are responsible for draining up to 90% of the mass from the ice sheet. It has been shown that Quaternary ice sheets were profoundly, and arguably catastrophically, influenced by the operation of transitory ice streaming.
Clark, C.D.   +2 more
openaire   +3 more sources

A new approach to inferring basal drag and ice rheology in ice streams, with applications to West Antarctic Ice Streams [PDF]

open access: yesJournal of Glaciology, 2020
AbstractDrag at the bed and along the lateral margins are the primary forces resisting flow in outlet glaciers. Simultaneously inferring these parameters is challenging since basal drag and ice viscosity are coupled in the momentum balance, which governs ice flow.
Meghana Ranganathan   +3 more
openaire   +6 more sources

How dynamic are ice-stream beds? [PDF]

open access: yesThe Cryosphere, 2017
Abstract. Projections of sea-level rise contributions from West Antarctica's dynamically thinning ice streams contain high uncertainty because some of the key processes involved are extremely challenging to observe. An especially poorly observed parameter is sub-decadal stability of ice-stream beds, which may be important for subglacial traction, till ...
Damon Davies   +8 more
openaire   +8 more sources

Ice flow in the northeast Greenland ice stream [PDF]

open access: yesAnnals of Glaciology, 2000
AbstractWe have measured ice flow and detailed topography in northeastern Greenland using satellite-based synthetic-aperture radar (SAR) interferometry. The subject of this study is the large ice stream that drains this quadrant of the ice sheet. A single SAR interferogram allows the measurement of one component of motion over a several-day-long ...
Joughin, IR, Fahnestock, M, Bamber, JL
openaire   +2 more sources

Ice-sheet surging and ice-stream formation [PDF]

open access: yesAnnals of Glaciology, 1996
A simplified model of ice-sheet behaviour is described. It combines the assumptions of rapid ice flow, high viscous activation energy and realistic sediment-based sliding dynamics to form a non-linear diffusion-type equation which can display relaxation oscillations analogous to those of surging glaciers, and which may be relevant to large-scale surges
C. Johnson, Andrew C. Fowler
openaire   +2 more sources

Accelerating ice flow at the onset of the Northeast Greenland Ice Stream [PDF]

open access: yesNature Communications, 2022
AbstractMass loss near the ice-sheet margin is evident from remote sensing as frontal retreat and increases in ice velocities. Velocities in the ice sheet interior are orders of magnitude smaller, making it challenging to detect velocity change. Here, we analyze a 35-year record of remotely sensed velocities, and a 6-year record of repeated GPS ...
Aslak Grinsted   +8 more
openaire   +4 more sources

Dynamic behaviour of rutford ice stream [PDF]

open access: yesAnnals of Glaciology, 1982
The grounding-line region of Rutford Ice Stream was surveyed from the ground during 1978–79 and 1979–80, and from the air in 1980–81. Maps of surface elevation and ice thickness of an area of 1 000 km2allow the grounding line to be delineated and show that the ice stream consists of several distinct fingers of thick ice trending parallel to the flow ...
Stephenson, S.N, Doake, C.S.M
openaire   +3 more sources

Contrasting the modelled sensitivity of the Amundsen Sea Embayment ice streams [PDF]

open access: yes, 2016
Present-day mass loss from the West Antarctic ice sheet is centred on the Amundsen Sea Embayment (ASE), primarily through ice streams, including Pine Island, Thwaites and Smith glaciers.
ANTONY J. PAYNE   +3 more
core   +3 more sources

Holocene ice-stream shutdown and drainage basin reconfiguration in northeast Greenland [PDF]

open access: yes, 2022
Reliable knowledge of ice discharge dynamics for the Greenland ice sheet via its ice streams is essential if we are to understand its stability under future climate scenarios.
Binder, Tobias   +11 more
core   +1 more source

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