Results 11 to 20 of about 217,482 (300)

Modelled subglacial floods and tunnel valleys control the life cycle of transitory ice streams [PDF]

open access: yesThe Cryosphere, 2018
Ice streams are corridors of fast-flowing ice that control mass transfers from continental ice sheets to oceans. Their flow speeds are known to accelerate and decelerate, their activity can switch on and off, and even their locations can shift ...
T. Lelandais   +6 more
doaj   +1 more source

Bed topography and marine ice-sheet stability

open access: yesJournal of Glaciology, 2022
This paper examines the effect of basal topography and strength on the grounding-line position, flux and stability of rapidly-sliding ice streams.
Olga V. Sergienko, Duncan J. Wingham
doaj   +1 more source

Repeated ice streaming on the northwest Greenland continental shelf since the onset of the Middle Pleistocene Transition [PDF]

open access: yesThe Cryosphere, 2020
Ice streams provide a fundamental control on ice sheet discharge and depositional patterns along glaciated margins. This paper investigates ancient ice streams by presenting the first 3D seismic geomorphological analysis of a major glacigenic succession ...
A. M. W. Newton   +4 more
doaj   +1 more source

Sensitivity of the Weddell Sea sector ice streams to sub-shelf melting and surface accumulation [PDF]

open access: yesThe Cryosphere, 2014
A recent ocean modelling study indicates that possible changes in circulation may bring warm deep-ocean water into direct contact with the grounding lines of the Filchner–Ronne ice streams, suggesting the potential for future ice losses from this sector ...
A. P. Wright   +10 more
doaj   +1 more source

Radar attenuation demonstrates advective cooling in the Siple Coast ice streams

open access: yesJournal of Glaciology, 2023
Ice streams are warmed by shear strain, both vertical shear near the bed and lateral shear at the margins. Warm ice deforms more easily, establishing a positive feedback loop in an ice stream where fast flow leads to warm ice and then to even faster flow.
Benjamin H. Hills   +4 more
doaj   +1 more source

Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set

open access: yesJournal of Glaciology, 2023
The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of understanding of this evolution hampers the ability to predict the effects of increasing temperatures ...
Signe H. Larsen   +5 more
doaj   +1 more source

A geomorphological overview of glacial landforms on the Icelandic continental shelf [PDF]

open access: yes, 2009
The availability of a bathymetric database that covers about 80% of the Icelandic shelf has made it possible to produce a geomorphological map of the glacial landforms.
Clark, C.D., Spagnolo, M.
core   +5 more sources

Stochastic ice stream dynamics [PDF]

open access: yesProceedings of the National Academy of Sciences, 2016
Significance Ice streams form the backbone of the flow field of ice sheets. They are known to exhibit a complex spatiotemporal dynamics, which is largely not well understood. Understanding the controls on such dynamics is crucial to sea level change projections as well as to the interpretation of paleorecords.
MANTELLI, ELISA   +2 more
openaire   +3 more sources

Thermomechanical modelling of the Scandinavian ice sheet: implications for ice-stream formation [PDF]

open access: yes, 1999
This work attempts to explain the fan-like landform assemblages observed in satellite images of the area covered by the former Scandinavian ice sheet (SIS). These assemblages have been interpreted as evidence of large ice streams within the SIS.
Baldwin, DJ, Payne, AJ
core   +2 more sources

Englacial Pore Water Localizes Shear in Temperate Ice Stream Margins [PDF]

open access: yes, 2019
The margins of fast‐moving ice streams are characterized by steep velocity gradients. Some of these gradients cannot be explained by a temperature‐dependent viscosity alone.
Haseloff, Marianne   +2 more
core   +2 more sources

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