Results 41 to 50 of about 401,804 (204)

Modeling Antarctic subglacial lake filling and drainage cycles [PDF]

open access: yesThe Cryosphere, 2016
The growth and drainage of active subglacial lakes in Antarctica has previously been inferred from analysis of ice surface altimetry data. We use a subglacial hydrology model applied to a synthetic Antarctic ice stream to examine internal controls on the
C. F. Dow   +3 more
doaj   +1 more source

Multianalytical provenance analysis of Eastern Ross Sea LGM till sediments (Antarctica): Petrography, geochronology, and thermochronology detrital data [PDF]

open access: yes, 2017
In order to reveal provenance of detrital sediments supplied by West Antarctic Ice Sheet (WAIS), 19 glaciomarine cores of Last Glacial Maximum age were analyzed from Eastern Ross Sea and Sulzberger Bay.
Andreucci, Benedetta   +4 more
core   +2 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.
Andrew C. Fowler   +3 more
openaire   +4 more sources

Ice fabric in an Antarctic ice stream interpreted from seismic anisotropy [PDF]

open access: yes, 2017
Here we present new measurements of an anisotropic ice fabric in a fast moving (377 ma−1) ice stream in West Antarctica. We use ∼6000 measurements of shear wave splitting observed in microseismic signals from the bed of Rutford Ice Stream, to show that ...
Alan F. Baird   +40 more
core   +3 more sources

High basal melting forming a channel at the grounding line of Ross Ice Shelf, Antarctica [PDF]

open access: yes, 2016
Antarctica's ice shelves are thinning at an increasing rate, affecting their buttressing ability. Channels in the ice shelf base unevenly distribute melting, and their evolution provides insight into changing subglacial and oceanic conditions.
Catania, Ginny   +6 more
core   +1 more source

Tidal controls on the flow of ice streams [PDF]

open access: yesGeophysical Research Letters, 2016
AbstractThe 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 that this has on the modeled response of ice streams to tides have, until now, not been ...
Rosier, Sebastian H.R.   +1 more
openaire   +3 more sources

Array processing in cryoseismology: a comparison to network-based approaches at an Antarctic ice stream [PDF]

open access: yesThe Cryosphere, 2023
Seismicity at glaciers, ice sheets, and ice shelves provides observational constraint on a number of glaciological processes. Detecting and locating this seismicity, specifically icequakes, is a necessary first step in studying processes such as basal ...
T. S. Hudson   +4 more
doaj   +1 more source

Spatiotemporal Dynamics of Ice Streams Due to a Triple-Valued Sliding Law [PDF]

open access: yes, 2010
We show that a triple-valued sliding law can be heuristically motivated by the transverse spatial structure of an ice-stream velocity field using a simple one-dimensional model.
Sayag, Roiy, Tziperman, Eli
core   +1 more source

Stream hydrology controls on ice cliff evolution and survival on debris-covered glaciers [PDF]

open access: yesEarth Surface Dynamics
Ice cliffs are melt hot spots that contribute disproportionately to melt on debris-covered glaciers. In this study, we investigate the impact of supraglacial stream hydrology on ice cliffs using in situ and remote sensing observations, streamflow ...
E. Petersen   +3 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   +1 more source

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