Results 1 to 10 of about 217,383 (201)
Modeling the elastic transmission of tidal stresses to great distances inland in channelized ice streams [PDF]
Geodetic surveys suggest that ocean tides can modulate the motion of Antarctic ice streams, even at stations many tens of kilometers inland from the grounding line.
J. Thompson, M. Simons, V. C. Tsai
doaj +6 more sources
The role of subtemperate slip in thermally driven ice stream margin migration [PDF]
The amount of ice discharged by an ice stream depends on its width, and the widths of unconfined ice streams such as the Siple Coast ice streams in West Antarctica have been observed to evolve on decadal to centennial timescales.
M. Haseloff +4 more
doaj +7 more sources
Frequency response of ice streams. [PDF]
Changes at the grounding line of ice streams have consequences for inland ice dynamics and hence sea level. Despite substantial evidence documenting upstream propagation of frontal change, the mechanisms by which these changes are transmitted inland are not well understood.
Williams CR, Hindmarsh RC, Arthern RJ.
europepmc +5 more sources
Modeling Ice Shelf/Ocean Interaction in Antarctica: A Review [PDF]
The most rapid loss of ice from the Antarctic Ice Sheet is observed where ice streams flow into the ocean and begin to float, forming the great Antarctic ice shelves that surround much of the continent.
Michael S. Dinniman +5 more
doaj +7 more sources
Antarctic palaeo-ice streams [PDF]
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.
Stephen J Livingstone +2 more
exaly +8 more sources
Tidal controls on the flow of ice streams [PDF]
The flow of many Antarctic ice streams is known to be significantly influenced by tides. In the past, modeling studies have implemented the tidal forces acting on a coupled ice stream/ice shelf system in a number of different ways, but the consequences ...
Sebastian H R Rosier +1 more
exaly +4 more sources
Subglacial hydrology and the formation of ice streams [PDF]
Richard F Katz
exaly +2 more sources
Ice-stream flow switching by up-ice propagation of instabilities along glacial marginal troughs [PDF]
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]
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
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

