... suggesting that Dansgaard - Oeschger events resulted from a combination of the effects of sea ice and ice shelves — structures that help define
the margins of ice sheets — to account for both the rapid and the slower parts of the cycle.
The margins of all ice sheets (including Greenland) are in retreat, and accumulation is negative over almost the whole of the West Antarctic sheet.
How and when is fresh water added to
the margins of ice sheets?
«The beds at
the margins of the ice sheet... are probably one of the least explored parts of Earth's surface,» said Ian Howat, a glaciologist at Ohio State University who did not participate in the research.
«The effort to use the old photographs to learn how
the margins of the ice sheet have changed is wonderful,» said Richard Alley, a glaciologist at Pennsylvania State University.
In northwest Greenland there is a 70 - km stretch of
the margin of the ice sheet called the Crimson Cliffs.
Satellite data show that
the margins of the ice sheet have darkened by as much as 5 % per decade since 2001.
«Since most ice sheet erosion occurs at
the margin of the ice sheet, that indicated times when the ice sheet retreated,» Cook said.
Not exact matches
The Dark Zone
of Greenland
ice sheet is a large continuous region on the western flank
of the
ice sheet; it is some 400 kilometers wide stretching about 100 kilometres up from the
margin of the
ice.
Tranter says he got the idea for Black and Bloom about four years ago, when he was working on the
margins of the Greenland
ice sheet and forgot his glacier goggles.
A study
of the demise
of the Laurentide
Ice Sheet that once covered Canada may help scientists better understand shrinking ice fields today — like this melting ice margin in Greenla
Ice Sheet that once covered Canada may help scientists better understand shrinking
ice fields today — like this melting ice margin in Greenla
ice fields today — like this melting
ice margin in Greenla
ice margin in Greenland.
A team from Rutgers University and the University
of Georgia, led by Asa Rennermalm
of Rutgers, measures meltwater runoff from the
ice sheet margin in Greenland during summer 2013.
So, now it seems that all
of the
margins of the Greenland
ice sheet are unstable.»
The full study, «Extensive dynamic thinning on the
margins of the Greenland and Antarctic
ice sheets,» was published in Nature (subs.
As more
ice are removed near the
ice margin, more intraplate earthquakes are induced and this positive feedback may explain the fast collapse
of ice sheets.
[this is useful, the pre-
ice age era, ~ 2.5 — 3.6 million years ago, last time CO2 levels were as high as today] In response to Pliocene climate,
ice sheet models consistently produce near - complete deglaciation
of the Greenland
ice sheet (+7 m) and West Antarctic
ice sheet (+4 m) and retreat
of the marine
margins of the Eastern Antarctic
ice sheet (+3 m)(Lunt et al., 2008; Pollard and DeConto, 2009; Hill et al., 2010), altogether corresponding to a global mean sea level rise
of up to 14 m.
The sea - level estimates are consistent with those from delta18O curves and numerical
ice sheet models, and imply a significant sensitivity
of the WAIS and the coastal
margins of the EAIS to orbital oscillations in insolation during the Mid-Pliocene period
of relative global warmth.
This conclusion was based on the fact that the WAIS
margin was ringed with stabilizing
ice shelves, and that much
of the
ice sheet is grounded below sea level.
«We were able to see for the first time that there is widespread thinning at the
margin of the Greenland
ice sheet throughout this region.
The
ice sheet is almost 2,400 kilometres long in a north - south direction, and its greatest width is 1,100 kilometres at a latitude
of 77 ° N, near its northern
margin.
The retreat sequence along the eastern
margin of the Laurentide
Ice Sheet is especially relevant for understanding climate variability.
What kind
of evidence would be an indicator
of ice -
sheet margin retreat?
Its key finding is that during the Pliocene there occurred a series
of long, warm intervals during which parts
of the East Antarctic
Ice -
Sheet margin retreated hundreds
of kilometres inland.
Pritchard, H. D., Arthern, R. J., Vaughan, D. G. & Edwards, L. A. Extensive dynamic thinning on the
margins of the Greenland and Antarctic
ice sheets.
The European Space Agency's CryoSat - 2 mission has enhanced Antarctic
ice sheet monitoring by including areas closer to the poles than earlier satellites, and by acquiring better data in moderately sloping areas, including
ice sheet margins where most
of the
ice loss occurs.
Coincident with rift formation was the sudden disintegration
of the
ice mélange that filled the northern shear
margin, resulting in
ice sheet detachment from this
margin.
Marine sediment record from the East Antarctic
margin reveals dynamics
of ice sheet recession.
Cartoon
of different paleoenvironmental scenarios
of sea
ice and
ice sheet extent at the East Siberian Continental
Margin / Southern Lomonosov Ridge area.
Such an extended
ice sheet associated with strong katabatic winds should have caused polynya - like open - water conditions in front
of the
ice sheet (Fig. 5a), resulting in increased fluxes
of phytoplankton,
ice algae and terrigenous matter as observed in the PS2757 - 8 record (Fig. 2c and Fig. 6, Scenario 2), i.e., a situation similar to that proposed for the Barents Sea continental
margin (Fig. 5a) 57, 58.
The Greenland
ice sheet terminates along this so - called grounded
ice margin near the town
of Ilulissat.
Timescales
of methane seepage on the Norwegian
margin following collapse
of the Scandinavian
Ice Sheet.
Joughin and others, 2008 observed that seasonal drainage
of meltwater to the glacier bed induces a uniform acceleration
of 50 — 150 meters / year over a ~ 300 km long section
of the West Greenland
margin that is not drained by outlet glaciers, causing a large fractional acceleration
of the interior
ice sheet but a small fractional change in the speed
of fast - moving outlet glaciers.
«This implies that changes at the
margin can affect the mass balance deep in the centre
of the
ice sheet,» said Dr Khan.
Observation
of a precipitation map (focused not on the outer
margin, but on the accumulation zone
of the
ice sheet) indicates that highest accumulation rates, over 40 cm per year, extend along the western side
of the
ice sheet to the southeast quadrant
of the
ice sheet.
Perhaps their most telling finding is that there is a definite difference between fast - flowing tidewater glaciers and slower parts
of the
ice -
sheet margins.
Research now shows that all
margins of the Greenland
ice sheet are now unstable — and [continue reading...]
Josh Willis, a lead NASA scientist for the Jason missions, which measure sea level rise from space and Ocean's Melting Greenland (OMG), is a passionate communicator about human - caused global warming.Come listen to a talk on what his team has found out about the role
of the oceans in
ice loss around the margins of the Greenland Ice She
ice loss around the
margins of the Greenland
Ice She
Ice Sheet.
Extensive dynamic thinning on the
margins of the Greenland and Antarctic
ice sheets.
At times, its southern
margin included the modern sites
of New York City and Chicago, and then followed quite precisely the present course
of the Missouri River up to the northern slopes
of the Cypress Hills, beyond which it merged with the Cordilleran
Ice Sheet.
The evidence comes from a remarkable find at the
margins of the Quelccaya
ice cap in Peru, the world's largest tropical
ice sheet.
1955 Richard F. Flint, «Rates
of Advance and Retreat
of the
Margin of the Late - Wisconsin
Ice Sheet.»