Results 61 to 70 of about 57,626 (157)
First description of subglacial megalineations from the late Paleozoic ice age in southern Africa.
We identify late Paleozoic ice age (LPIA) subglacial megalineations from field and geospatial imagery of the Twyfelfontein area of northern Namibia, and present the results of a geomorphometric analysis of those data.
Graham D Andrews +3 more
doaj +1 more source
Accelerating ice flow at the onset of the Northeast Greenland Ice Stream. [PDF]
Grinsted A +8 more
europepmc +1 more source
Crevasse refreezing and signatures of retreat observed at Kamb Ice Stream grounding zone. [PDF]
Lawrence JD +15 more
europepmc +1 more source
Extensive inland thinning and speed-up of Northeast Greenland Ice Stream. [PDF]
Khan SA +9 more
europepmc +1 more source
Migratory earthquake precursors are dominant on an ice stream fault. [PDF]
Barcheck G +5 more
europepmc +1 more source
Ice-Shelf Response to Ice-stream Discharge Fluctuations: III. The Effects of Ice-stream Imbalance on the Ross Ice Shelf, Antarctica [PDF]
AbstractA numerical simulation of the Ross Ice Shelf, Antarctica, in which discharge from Ice Streams A-E is changed suddenly between extreme states, is used to investigate ice-shelf thickness and flow anomalies generated by ice-stream transience.
openaire +1 more source
Abnormal sea-ice retreat over the Barents Sea during early winter has been considered a leading driver of recent midlatitude severe winters over Eurasia. However, causal relationships between such retreat and the atmospheric circulation anomalies remains
Kazutoshi Sato +2 more
doaj +1 more source
Topographic and geologic controls on the Northeast Greenland Ice Stream
The Northeast Greenland Ice Stream (NEGIS) is an elongated feature extending ∼600 km into the interior of the Greenland Ice Sheet. Here, we investigate detailed subglacial topography along the length of the NEGIS to ascertain the characteristics of the ...
Charlotte M. Carter +7 more
doaj +1 more source
Ice streams are bounded by abrupt transitions in speed called shear margins. Some shear margins are fixed by subglacial topography, but others are thought to be self‐organizing, evolving by thermal feedback to ice viscosity and basal drag which govern ...
N. Holschuh +2 more
doaj +1 more source

