Ice flow velocity as color over SAR amplitude imagery of Jakobshavn Isbræ in a) February 1992 b) October 2000.
Researchers used RADARSAT synthetic aperture radar to map
ice flow velocity over Greenland for the winters of 2000 - 2001 and 2005 - 2006.
Not exact matches
Ice velocity mapping of
Ice Streams D, F, and the Shirase Coast:
flow dynamics and change.
«
Ice velocities near a relict
flow feature on Siple Dome,» Antarctic Journal of the United States, XXIX (5), p. 62 - 66.
Leakage of the Greenland
Ice Sheet through accelerated ice flow AU: * Rignot, E AF: Jet Propulsion Laboratory / Caltech, MS 300-319 4800 Oak Grove Drive, Pasadena, ca 91109 - 8099 United States AB: A map of coastal velocities of the Greenland ice sheet was produced from Radarsat - 1 acquired during the background mission of 2000 and combined with radio echo sounding data to estimate the ice discharge from the ice she
Ice Sheet through accelerated
ice flow AU: * Rignot, E AF: Jet Propulsion Laboratory / Caltech, MS 300-319 4800 Oak Grove Drive, Pasadena, ca 91109 - 8099 United States AB: A map of coastal velocities of the Greenland ice sheet was produced from Radarsat - 1 acquired during the background mission of 2000 and combined with radio echo sounding data to estimate the ice discharge from the ice she
ice flow AU: * Rignot, E AF: Jet Propulsion Laboratory / Caltech, MS 300-319 4800 Oak Grove Drive, Pasadena, ca 91109 - 8099 United States AB: A map of coastal
velocities of the Greenland
ice sheet was produced from Radarsat - 1 acquired during the background mission of 2000 and combined with radio echo sounding data to estimate the ice discharge from the ice she
ice sheet was produced from Radarsat - 1 acquired during the background mission of 2000 and combined with radio echo sounding data to estimate the
ice discharge from the ice she
ice discharge from the
ice she
ice sheet.
The current
flow speeds at the terminus are too fast to be caused solely by internal deformation of the
ice, implying that an increase in basal sliding forced by additional meltwater production is the probable cause of the
velocity increases.
Terran: An examination of a map of glacier
velocity for either the Pine Island presented in this post or of the
ice streams feeding the Ross Ice Shelf indicate that most of the ice sheet region is not a fast flow regi
ice streams feeding the Ross
Ice Shelf indicate that most of the ice sheet region is not a fast flow regi
Ice Shelf indicate that most of the
ice sheet region is not a fast flow regi
ice sheet region is not a fast
flow region.
Greenland
flow variability from
ice - sheet wide
velocity mapping.
Changes on fast -
flow marine - terminating glaciers contrast with steady
velocities on
ice - shelf — terminating glaciers and slow speeds on land - terminating glaciers.
Greenland
flow variability from
ice - sheet - wide
velocity mapping.
If you watch the NRL Hycom animations (sequences of daily arctic
ice concentration) or look at
velocity maps, a lot of the arctic cap
flows south.
«With most glaciers that are moving
ice from the land into the sea and causing sea level rise in Greenland, the majority of their
velocity appears to be due to the
flow rather than the sliding,» he said.
New research, using
ice velocity data from satellites such as ESA's heritage Envisat, has revealed that there is a critical point where these shelves act as a safety band, holding back the
ice that
flows t...
We map present - day Antarctic - wide surface
velocities using Landsat 7 and 8 imagery spanning 2013 — 2015 and compare to earlier estimates derived from synthetic aperture radar, revealing heterogeneous changes in
ice flow since ∼ 2008.
In contrast, Joughin and Tulaczyk's analysis takes advantage of the much - expanded database available from
ice -
flow velocity measurements obtained using Interferometric Synthetic Aperture Radar.