Dust trapped over the centuries has become concentrated at
the melting edge of the ice sheet.
Not exact matches
Melting near the
edges of the Greenland
ice sheet, where the surface is below 4,000 feet, causes about half
of its annual
ice loss.
The great
ice sheets of Greenland and Antarctica, which rise to over 13,000 feet above sea level, accumulate
ice over most
of their surfaces and
melt only at their lower elevations near the
edges.
These new measurements confirm what some
of the more pessimistic scientists thought: The
melting along the crucial
edges of the two major
ice sheets is accelerating and is in a self - feeding loop.
«Most
ice cores are collected from the middle
of the
ice sheet where it rarely ever
melts, or on the
ice sheet edge where the meltwater flows into the ocean,» Karina Graeter, the lead author
of the study as a graduate student in Dartmouth's Department
of Earth Sciences, said in a statement.
Other factors would include: — albedo shifts (both from
ice > water, and from increased biological activity, and from
edge melt revealing more land, and from more old dust coming to the surface...); — direct effect
of CO2 on
ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on
ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; —
melting of sea
ice shelf increasing mobility
of glaciers; — sea water getting under parts
of the
ice sheets where the base is below sea level; —
melt water lubricating the
ice sheet base; — changes in ocean currents -LRB-?)
Thomas, I appreciate that they are imperfect things to compare, but have you ever seen pictures
of the
ice pack near the
edge of the
ice sheet where the
melting is happening fastest?
So, as the leading
edge melts, this deformation and filling would be first observed as a thinning
of the
sheet and, in particular, the trunk or main
ice stream channel, as well as an acceleration
of the stream.
Around the
edges of the
ice sheet, though, there is accelerated
melting.
Generally yes, but there has been a lot
of new information learned since the IPCC Third Assessment Report (e.g., on trends in hurricane intensity, the accelerated
melting back
of Arctic sea
ice, the intensifying deterioration of the edges of the Greenland Ice Sheet, etc.) and Gore's presentation of the science has been updated to account for these, drawing from what are the really highly reviewed and high quality papers by leading scientis
ice, the intensifying deterioration
of the
edges of the Greenland
Ice Sheet, etc.) and Gore's presentation of the science has been updated to account for these, drawing from what are the really highly reviewed and high quality papers by leading scientis
Ice Sheet, etc.) and Gore's presentation
of the science has been updated to account for these, drawing from what are the really highly reviewed and high quality papers by leading scientists.
-- Susan Solomon, Nature The Long Thaw is written for anyone who wishes to know what cutting -
edge science tells us about the modern issue
of global warming and its effects on the pathways
of atmospheric chemistry, as well as global and regional temperatures, rainfall, sea level, Arctic sea -
ice coverage,
melting of the continental
ice sheets, cyclonic storm frequency and intensity and ocean acidification.
If a relatively small chunk
of ice currently plugging the
edge of an
ice sheet in Antarctica were to
melt, it could release massive amounts
of ice into the ocean that would significantly increase global sea level for the next 10,000 years, according to a new report.
In a new study, Box and a team
of researchers describe the decline in
ice sheet reflectivity and the reasons behind it, noting that if current trends continue, the area
of ice that
melts during the summer season is likely to expand to cover all
of Greenland for the first time in the observational record, rather than just the lower elevations at the
edges of the continent, as is the case today.
In fact, 2005 looks to feature the greatest amount
of melting of the
edge of the
ice sheet in Greenland in about 30 years (or more):
Over the course
of several years, turbulent water overflow from a large
melt lake carved this 60 - foot - deep (18.3 meter - deep) canyon in Greenland's
Ice Sheet (note people near left
edge for scale).
This ocean will be incredibly important for sea level rise, because the easiest way to destabilise the Antarctic
Ice Sheet is to warm up the ocean and melt the ice shelves (the edges of the ice sheet which extend over the ocean) from bel
Ice Sheet is to warm up the ocean and melt the ice shelves (the edges of the ice sheet which extend over the ocean) from b
Sheet is to warm up the ocean and
melt the
ice shelves (the edges of the ice sheet which extend over the ocean) from bel
ice shelves (the
edges of the
ice sheet which extend over the ocean) from bel
ice sheet which extend over the ocean) from b
sheet which extend over the ocean) from below.
An
ice sheet teetering on the
edge of melting away is going to have a huge response because just a little extra energy changes the albedo.
The
edges of Greenland's 1.7 - million - km2
ice sheet regularly
melt in summer, even in years when the
ice sheet as a whole grows because
of snowfall in its higher, colder center.
But because the
ice sheet is steep at its
edges but flatter toward the middle, each successive degree
of warming exposes a larger area
of ice to
melting than the last.
Each increase in temperature drives the upper
edge of the
melt zone farther inland and higher up the
ice sheet.