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Antarctic Palaeo-Ice Streams [PDF]

open access: yesEarth-Science Reviews, 2012
We review the geomorphological, sedimentological and chronological evidence for palaeo-ice streams on the continental shelf of Antarctica and use this information to investigate basal conditions and processes, and to identify factors controlling grounding-line retreat.
Andreas Vieli   +2 more
exaly   +8 more sources

Ice Streams of the Laurentide Ice Sheet [PDF]

open access: yesGéographie physique et Quaternaire, 2006
Ice streams had a major influence on the configuration and the stability of the Laurentide Ice Sheet. Their identification is crucial for an understanding of ice sheet behaviour and their importance is reflected by the recent increase in paleo-ice stream research.
Winsborrow, Monica C.M.   +2 more
openaire   +4 more sources

Stochastic Ice Stream Dynamics [PDF]

open access: yesProceedings of the National Academy of Sciences of the United States of America, 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.
Elisa Mantelli   +2 more
exaly   +4 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, 2021
Drag 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 ...
Meghana Ranganathan   +3 more
doaj   +6 more sources

Subglacial Hydrology and the Formation of Ice Streams [PDF]

open access: yesProceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 2014
Antarctic ice streams are associated with pressurized subglacial meltwater but the role this water plays in the dynamics of the streams is not known. To address this, we present a model of subglacial water flow below ice sheets, and particularly below ice streams.
Richard F. Katz, A C Fowler
exaly   +4 more sources

Chaotic variability in a model of coupled ice streams [PDF]

open access: yes
Regions of fast-flowing ice in ice sheets, known as ice streams, have been theorized to be able to exhibit build-up/surge oscillatory variability due to thermomechanical coupling at the base of the ice.
Peter Ditlevsen (21829829)   +2 more
core   +8 more sources

Ice-stream flow switching by up-ice propagation of instabilities along glacial marginal troughs [PDF]

open access: yesThe Cryosphere, 2019
Ice-stream networks constitute the arteries of ice sheets through which large volumes of glacial ice are rapidly delivered from the continent to the ocean.
E. Brouard, P. Lajeunesse
doaj   +1 more source

Subglacial hydrological control on flow of an Antarctic Peninsula palaeo-ice stream [PDF]

open access: yesThe Cryosphere, 2019
Basal hydrological systems play an important role in controlling the dynamic behaviour of ice streams. Data showing their morphology and relationship to geological substrates beneath modern ice streams are, however, sparse and difficult to collect.
R. D. Larter   +13 more
doaj   +1 more source

‘Stable’ and ‘unstable’ are not useful descriptions of marine ice sheets in the Earth's climate system

open access: yesJournal of Glaciology, 2023
Investigations of the time-dependent behavior of marine ice sheets and their sensitivity to basal conditions require numerical models because existing theoretical analyses focus only on steady-state configurations primarily with a power-law basal shear ...
Olga Sergienko, Marianne Haseloff
doaj   +1 more source

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

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