Bamber has recalculated the critical threshold temperature
for ice sheet melting by forcing two surface mass balance models with real future climate.
The biggest problem seems to be
for ice sheet melt, in the discrepancy between the paleoevidence and the models, with models producing rates of melting far below both the paleoevidence and current observations.
Not exact matches
Things I changed: - cut the sugar by about half, using mostly dark brown sugar
for the molasses kick - scratched the nutmeg and allspice but added about 1/3 extra of all of the other spices and also added nearly a tsp of ground cardamon - replaced the veggie oil with
melted leaf lard - scratched the raisins - baked it on a deep
sheet for only ~ 20 minutes - just barely until firm to the touch - then cut that
sheet into three layers - replaced the
icing with my own 16 ounce cream cheese, 8 ounce butter, ~ 6 ounce heavy cream, ~ 5 ounce honey, 1 tsp vanilla combo - toasted the coconut before dressing the cake.
According to the Center
for Remote Sensing of
Ice Sheets (CReSIS), an NSF Science and Technology Center led by the University of Kansas, the melt from Greenland's ice sheet contributes to global sea level rise at a rate of 0.52 millimeters annual
Ice Sheets (CReSIS), an NSF Science and Technology Center led by the University of Kansas, the
melt from Greenland's
ice sheet contributes to global sea level rise at a rate of 0.52 millimeters annual
ice sheet contributes to global sea level rise at a rate of 0.52 millimeters annually.
Considering that the Greenland and Antarctic
ice sheets span more than 1.7 million and 14 million square kilometers, respectively, while containing 90 % of the world's freshwater
ice supply,
melting of
ice shelves could be catastrophic
for low - lying coastal areas.
«The influence of distant forest fires on
melt events on the Greenland
ice sheet is inherently challenging to demonstrate and these clear chemical results provide another line of evidence
for this connection,» said Diane McKnight, a CU Boulder professor and a co-author of the study.
The Antarctic
ice sheet was expected to grow, with increased snowfall compensating
for melting around the edges.
For example, heat waves were particularly severe, droughts were extensive in tropical forests, and
melting of the Greenland
ice sheet accelerated in association with shifts in the 8 - day maximum temperature.
Recent modelling by researchers from the Potsdam Institute
for Climate Impact Research in Germany, as well as studies of past climate, suggest that the planet will soon have warmed enough to
melt Greenland's
ice sheet entirely — if it hasn't already become warm enough.
This could have significant implications
for Antarctica's
ice shelves and
ice sheets, with previous research showing that even small increases in ocean temperatures can substantially increase
melt rates around the Peninsula.
Operation IceBridge, NASA's airborne survey of polar
ice, is flying in Greenland
for the second time this year, to observe the impact of the summer
melt season on the
ice sheet.
Their results show that East Greenland has been actively scoured by glacial
ice for much of the last 7.5 million years — and indicate that the
ice sheet on this eastern flank of the island has not completely
melted for long, if at all, in the past several million years.
Pettersen is hopeful that, with more data analysis over longer periods of time, researchers will find more answers yet to account
for the
melting ice sheet and the subsequent sea level rise that has already had an impact on regions across the planet.
For instance, it was previously thought that it would take hundreds of years for the Greenland ice sheet to melt right the way throu
For instance, it was previously thought that it would take hundreds of years
for the Greenland ice sheet to melt right the way throu
for the Greenland
ice sheet to
melt right the way through.
Your feature on uneven global distribution of sea level rise as
ice sheets melt highlights a double whammy
for northern...
For instance, researchers may have a limited time to survey coastal archaeological sites threatened by erosion, to sample
melting ice sheets holding clues to past climates, and to document so - called thermokarst lakes, which are formed by meltwater from permafrost.
Box pointed to nearly
ice -
sheet - wide
melting on Greenland, with extensive surface
melting documented
for first time at the highest elevations of
ice sheet, and the longest
melt season since satellite observations began in 1979.
Melting of glaciers and the massive
ice sheets of Greenland and Antarctica will combine
for a rise in sea levels of 25 meters, or about 80 feet.
Rather than start remediation now, Colgan said, «It really becomes a situation of waiting until the
ice sheet has
melted down to almost expose the wastes that anyone should advocate
for site remediation.»
For millennia, Greenland's
ice sheet reflected sunlight back into space, but satellite measurements in recent years suggest the bright surface is darkening, causing solar heat to be absorbed and surface
melting to accelerate.
Also in the mid-1990s, another group of scientists proposed the now widely accepted mechanism
for how lakes can form under glaciers: Heat radiating from Earth's interior is trapped under the thick, insulating
ice sheet, and pressure from the weight of all the
ice above it lowers the
melting point of the
ice at the bottom.
The international team of co-authors, led by Peter Clark of Oregon State University, generated new scenarios
for temperature rise, glacial
melting, sea - level rise and coastal flooding based on state - of - the - art climate and
ice sheet models.
For the first time, ocean data from Northeast Greenland reveals the long - term impact of the
melting of the Greenland
ice sheet.
Greenland's
ice sheet melts and sends large amounts of fresh water into the coastal waters, where it is of major importance
for local production but potentially also
for global ocean currents.
It could lead to a massive increase in the rate of
ice sheet melt, with direct consequences
for global sea level rise.»
A new study led by the University of Texas Institute
for Geophysics has found that wind over the ocean off the coast of East Antarctica causes warm, deep waters to upwell, circulate under Totten
Ice Shelf, and melt the fringes of the East Antarctic ice sheet from bel
Ice Shelf, and
melt the fringes of the East Antarctic
ice sheet from bel
ice sheet from below.
Totten Glacier, the largest glacier in East Antarctica, is being
melted from below by warm water that reaches the
ice when winds over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice of the East Antarctic Ice She
ice when winds over the ocean are strong — a cause
for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the
ice of the East Antarctic Ice She
ice of the East Antarctic
Ice She
Ice Sheet.
«Based on the UN climate panel's report on sea level rise, supplemented with an expert elicitation about the
melting of the
ice sheets,
for example, how fast the
ice on Greenland and Antarctica will
melt while considering the regional changes in the gravitational field and land uplift, we have calculated how much the sea will rise in Northern Europe,» explains Aslak Grinsted.
Contrary to what you might expect, the third IPPC report predicted that global warming would most likely lead to a thickening of the
ice sheet over the next century, with increased snowfall compensating
for any
melting cause by warming.
Sea levels would creep up nearly six inches as a result of that extra heat, with any additional rise due to
melting ice sheets unaccounted
for in the study's calculations.
The
melting of the
ice sheet is responsible
for a maximum of a third of this.
Melting ice sheets could raise sea levels high enough to flood coastal areas around the globe by the end of the century, according to scientists gathering in Denmark today
for a three - day climate - change conference.
Some have wondered whether the
melting of the Cordilleran
Ice Sheet caused the Younger Dryras cooling, but it's unlikely; the cooling started too early
for that to be true, according to the study.
These findings suggest that Greenland's glaciers have been experiencing increasing
ice loss
for at least three decades — a result that may reinforce scientists» concerns over the stability of the
melting ice sheet.
Some scientists believe the
ice sheet experienced significant
melting during the relatively warmer conditions of the Pliocene, while others think it has remained almost entirely frozen
for the last 14 million years.
Recent projections show that
for even the lowest emissions scenarios, thermal expansion of ocean waters21 and the
melting of small mountain glaciers22 will result in 11 inches of sea level rise by 2100, even without any contribution from the
ice sheets in Greenland and Antarctica.
Shifting winds have helped drive West Antarctica's
ice sheet melting for millennia, according to a new analysis that could help scientists better anticipate sea - level rise.
«This makes future projections extremely challenging — anything from 10 centimeters to over a meter is currently on the table
for sea - level rise due to
melting ice sheets,» Landerer said in an email.
Meanwhile, atmospheric greenhouse gas levels grow,
ice sheets melt, hurricanes become more ferocious, and the day of reckoning
for the Earth looms closer.
The warming of the WAIS is most worrisome (at least
for this century) because it's going to disintegrate long before the East Antarctic
Ice Sheet does «'' since WAIS appears to be
melting from underneath (i.e. the water is warming, too), and since, as I wrote in the «high water» part of my book, the WAIS is inherently less stable:
«The
ice sheets in the north
melted completely about 8,000 years ago and it will take 20,000 years
for the crust to rebound.
For example,
ice loss in far - off West Antarctica will have more profound impacts in Scandinavia than it will in nearby Australia, while right now
melting Alaskan glaciers contribute more to sea - level rise in the Baltic than the Greenland
ice sheet.
So researchers need to look elsewhere
for clues of
ice sheet melt in the more distant past.
When projecting how sea levels could rise over the coming centuries, one of the most difficult factors
for scientists to gauge is how much of the Earth's vast
ice sheets will
melt, and how quickly.
From 1992 to 2003, the decadal ocean heat content changes (blue), along with the contributions from
melting glaciers,
ice sheets, and sea
ice and small contributions from land and atmosphere warming, suggest a total warming (red)
for the planet of 0.6 ± 0.2 W / m2 (95 % error bars).
Estimates from the National Snow and
Ice Data Center indicate that roughly half the ice sheet's surface is melting, well above the average of around 25 percent for this time of ye
Ice Data Center indicate that roughly half the
ice sheet's surface is melting, well above the average of around 25 percent for this time of ye
ice sheet's surface is
melting, well above the average of around 25 percent
for this time of year.
Scientific knowledge input into process based models has much improved, reducing uncertainty of known science
for some components of sea - level rise (e.g. steric changes), but when considering other components (e.g.
ice melt from
ice sheets, terrestrial water contribution) science is still emerging, and uncertainties remain high.
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«What the situation suggests
for Greenland
ice melt summer 2016 is some thermal erosion of the «cold content» of the snow overlying the
ice sheet, meaning less heat needed to «ripen'the snow to the
melting point,» Box said.
Emerging from a winter that has had staggeringly warm Arctic temperatures, scientists monitoring the vast Greenland
ice sheet announced Tuesday that it is experiencing a record - breaking level of
melt for so early in the season.