Results 111 to 120 of about 917,323 (294)
The dominant mass-loss process on the Antarctic Peninsula has been ice-shelf collapse, including the Larsen A Ice Shelf in early 1995. Following this collapse, there was rapid speed up and thinning of its tributary glaciers.
SAM ROYSTON, G. HILMAR GUDMUNDSSON
doaj +1 more source
. Ocean-induced basal melting is responsible for much of the Amundsen Sea Embayment ice loss in recent decades, but the total magnitude and spatiotemporal evolution of this melt is poorly constrained.
D. Shean +4 more
semanticscholar +1 more source
The MOSAiC ice floe: sediment-laden survivor from the Siberian shelf
. In September 2019, the research icebreaker Polarstern started the largest multidisciplinary Arctic expedition to date, the MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) drift experiment. Being moored to an ice floe for
T. Krumpen +37 more
semanticscholar +1 more source
Centurial‐millenial ice‐rafted debris pulses from ablating marine ice sheets [PDF]
We use an ice‐sheet model to show that (i) margins of marine ice‐sheets can be expected to be frozen to the bed, except where ice‐streams discharge; (ii) 20–50km retreats induced by ablation rates of 2 m/yr provide sufficient debris flux through the ...
Hindmarsh, Richard C.A., Jenkins, Adrian
core +1 more source
Direct measurements of ice-shelf flexure caused by surface meltwater ponding and drainage
Global sea-level rise is caused, in part, by more rapid ice discharge from Antarctica, following the removal of the restraining forces of floating ice-shelves after their break-up.
A. Banwell +4 more
semanticscholar +1 more source
Seasonal and spatial variations in the ocean-coupled ambient wavefield of the Ross Ice Shelf [PDF]
© The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Baker, M. G., Aster, R. C., Anthony, R. E., Chaput, J., Wiens, D. A., Nyblade, A., Bromirski, P.
Anthony, Robert E. +8 more
core +1 more source
Brine, englacial structure and basal properties near the terminus of McMurdo Ice Shelf, Antarctica
We collected ~1300 km of ground-penetrating radar profiles over McMurdo Ice Shelf, Antarctica, using frequencies between 40 and 400 MHz to determine extent, continuity and depth to the brine.
S. Campbell +3 more
doaj +1 more source
A Speed Limit on Ice Shelf Collapse Through Hydrofracture
Increasing surface melt has been implicated in the collapse of several Antarctic ice shelves over the last few decades, including the collapse of Larsen B Ice Shelf over a period of just a few weeks in 2002.
A. Robel, A. Banwell
semanticscholar +1 more source
Tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow [PDF]
GPS measurements reveal strong modulation of horizontal ice shelf and ice stream flow at a variety of tidal frequencies, most notably a fortnightly (Msf) frequency not present in the vertical tides themselves. Current theories largely fail to explain the
Gudmundsson, Hilmar, Rosier, Sebastian
core +1 more source
How Accurately Should We Model Ice Shelf Melt Rates?
Assessment of ocean‐forced ice sheet loss requires that ocean models be able to represent sub‐ice shelf melt rates. However, spatial accuracy of modeled melt is not well investigated, and neither is the level of accuracy required to assess ice sheet loss.
Daniel Goldberg +4 more
semanticscholar +1 more source

