«Radar observations of a relict
ice stream margin traversing Siple Dome, Antarctica,»» Antarctic Journal of the United States, XXX (5), (in press).
Not exact matches
Changes in the
margin of
ice stream C, Antarctica.
Present
ice streams draining the Greenland and Antarctic
ice sheets have characteristic concave surface profiles produced when slow interior sheet flow is downdrawn by fast
stream flow near
ice - sheet
margins.
For the LIM experiment, we enlisted James Fastook to incorporate the marine instability mechanism published by Robert Thomas in 1977 to make grounded
ice margins retreat when
ice downdrawn by
ice streams became thin enough to become afloat along the WAIS marine
margins.
The
margins usually slope more steeply, and most
ice is discharged through fast - flowing
ice streams or outlet glaciers, in some cases into the sea or into
ice shelves floating on the sea.