van den Broeke, M. R., C. J. P. P. Smeets, and R. S. W. van de Wal (2011), The seasonal cycle and interannual variability of surface energy balance and melt
in the ablation zone of the west Greenland ice sheet, Cryosphere, 5, 377 — 390.
A recent article in Science has an alarming title: «Large and Rapid Melt - Induced Velocity Changes
in the Ablation Zone of the Greenland Ice Sheet.»
It explains why, in glaciers that are mostly cold, the ice at high altitude in the accumulation zone is usually warmer than the ice at lower altitude
in the ablation zone.
The accumulation area decreased by 24.8 %, while ablation area increased by 17.7 % with nearly 6 % increase in debris - cover surface
in ablation zone in 1958 to 2011.
The North Cascade Glacier Climate Project (NCGCP), utilizes the highest density of measurements 240 points / km2 in the accumulation zone and 10 points / km2
in the ablation zone.
«Large and Rapid Melt - Induced Velocity Changes
in the Ablation Zone of the Greenland Ice Sheet.»
This positive feedback gives rise to high concentrations of impurities
in the ablation zones in particular.
Not exact matches
In effect, this UAV survey across the ablation zone of the ice sheet perfectly bridges the gap between people on the ground studying what's under their feet in just one part of the ice sheet, and the satellite data that shows what's going on across the entire ice shee
In effect, this UAV survey across the
ablation zone of the ice sheet perfectly bridges the gap between people on the ground studying what's under their feet
in just one part of the ice sheet, and the satellite data that shows what's going on across the entire ice shee
in just one part of the ice sheet, and the satellite data that shows what's going on across the entire ice sheet.
In the paper the authors argue that there is no evidence for a speed up of the ice marginal
zone due to enhanced
ablation rates, which by some people was explained as if Greenland was not contributing to sea level change any more.
Prolonged thinning of the
ablation zone (as shown
in Fig. 8) causes an additional warming for these areas, which should be lower
in altitude if the topography could evolve during the simula - tion.
In Glacier National Park, North Cascades, Helm Glacier and Place Glacier frequent loss of the entire snowcover by the end of the ablation season has become commonplace (WGMS, 2005 The result is in net ablation throughout the accumulation area causing thinning of the glacier in the accumulation zon
In Glacier National Park, North Cascades, Helm Glacier and Place Glacier frequent loss of the entire snowcover by the end of the
ablation season has become commonplace (WGMS, 2005 The result is
in net ablation throughout the accumulation area causing thinning of the glacier in the accumulation zon
in net
ablation throughout the accumulation area causing thinning of the glacier
in the accumulation zon
in the accumulation
zone.
On Columbia, Daniels, Foss, Ice Worm, Lower Curtis, Sholes, and Yawning Glacier thinning is not notably less
in the accumulation
zone than the
ablation zone, indicating disequilibrium (Pelto, 2006).
This is their sensitivity Achilles Heel: relatively little increases
in melt can expand the
ablation zone appreciably given the low surface slopes and low accumulation rates.
But Phillips and his co-authors are more interested
in cryohydrologic warming of the
ablation zone.
The surface mass balance observations similarly indicate that the ELA has migrated upwards at a rate of 44 m / a over the 1997 — 2011 period
in West Greenland, resulting
in a more than doubling of the
ablation zone width during this period...»
To date, the amount of black carbon
in the region of the GrIS that is losing mass, known as the
ablation zone, has not been quantified.
Although some scientists have hypothesized that dust may be darkening the
ablation zone in southwest Greenland
in particular, nobody has quantified the relative roles of black carbon, dust, and other darkening agents
in these regions.
We also need
in situ measurements
in the GrIS's
ablation zone that can distinguish the relative contributions of different impurity types (e.g., black carbon, dust, algae) to albedo reduction as well as models that accurately simulate the GrIS surface energy balance and mass balance.