With
this much ice melt potentially being dumped into the sea, the global sea level could rise by as much as 4 feet (1.2 meters).
How
much ice melted on Greenland last summer?
In addition, the enhanced detail of where and how
much ice melted allowed the researchers to estimate that the annual acceleration in ice loss is much lower than previous research has suggested, roughly increasing by 8 billion tons every year.
Not exact matches
Greenland's coastal glaciers and
ice caps have passed a pivotal tipping point — a new study concludes that they've
melted so
much that they're now past the point of no return, and it's unlikely in current conditions that they'll be able to regrow the
ice they've lost.
On top of all this, all electric power generation produces heat, and too
much generation will raise the earth's temperature, possibly enough to cause partial
melting of the polar
ice caps and wreak havoc on the world's ecosphere.
Gore begins with hero scientists like Roger Revelle, who first began to imagine the magnitude of this tragedy, and continues through the latest scientific findings, like last fall's revelation that the
ice over Greenland seems to be
melting much faster than anyone had predicted — news that carries potentially cataclysmic implications for the rate of sea - level rise.
This will keep your
ice from
melting as
much!
Coconut milk is
much creamier, almond milk is a little thick but bland if you go for the unsweetened kind, and flax milk tastes like
melted vanilla
ice cream.
Even directly out of the freezer, an oil - based cube of herbs will soften and
melt much faster than a
ice cube of equivalent size.
Much like any
ice cream cake, this recipe will
melt when removed from the freezer.
Add coconut milk
ice cubes and blend until just smooth and no
ice cube chunks remain (don't blend too
much or the
ice will begin to
melt, and you'll lose that thick milkshake consistency).
It's important to let the vegan cream cheese sit out at least 10 minutes before you mix in the sweetener so it has enough time to
melt a little which will make the whole
icing process
much easier.
This brownie was a survivor — while the
icing melted fairly quickly, even after six minutes the cake part was holding strong and still retaining
much of its original form.
All I'm thinking is if you left it out any longer it'd
melt... and that's too
much ice cream for one person... so, I think I should come over and help you eat it up!
In Alaska and eastern Siberia, she and her colleagues are cataloging the Arctic freezer's carbon contents, trying to understand how
much will be converted to methane as the
ice melts.
And that is because especially lining the peninsula as that
ice melts, it makes that continent
much more accessible to exploitation, oil drilling, precious mineral searches, which is suddenly going on now.
It is the major factor governing how
much incoming solar radiation is used to
melt the
ice and is the main positive feedback in Arctic climate change.
«Instead of emerging at the surface,
much of that heat is
melting the
ice shelves,» Hansen says, producing more fresh water and amplifying the feedback.
... It's not so
much air temperatures but warmer water underneath that is
melting these
ice sheets.»
«The fact that a large portion of the western flank of the Greenland
ice sheet has become dark means that the
melt is up to five times as
much as if it was a brilliant snow surface.»
«The planet is in its danger zone because we've poured too
much carbon into the atmosphere, and we're starting to see signs of real trouble:
melting ice caps, rapidly spreading drought.
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.
Velicogna and her colleagues also measured a dramatic loss of Greenland
ice, as
much as 38 cubic miles per year between 2002 and 2005 — even more troubling, given that an influx of fresh
melt water into the salty North Atlantic could in theory shut off the system of ocean currents that keep Europe relatively warm.
Take Holland: It will be
much more heavily influenced by Antarctic
ice melt than by falling sea levels around Greenland, says Jerry Mitrovica, a geophysicist and sea level modeler at Harvard University.
But scientists increasingly attribute
much of the observed grounding line retreat — particularly in West Antarctica — to the influence of warmer ocean water seeping beneath the
ice shelves and lapping against the bases of glaciers,
melting the
ice from the bottom up.
Within a few hundred years sea levels in some places had risen by as
much as 10 meters — more than if the
ice sheet that still covers Greenland were to
melt today.
All told, if the eastern and western Antarctic
ice shelves were to
melt completely, they would raise sea levels by as
much as 230 feet (70 meters); the collapse of smaller shelves like Larsen B has sped up the flow of glaciers behind them into the sea, contributing to the creeping up of high tide levels around the world.
In Greenland this doesn't happen
much because the water drains away through big channels like the mega-canyon, so
melting ice sheets there tend not to drive rapid sea level rises.
Schimdt has found evidence that warm ocean currents and convective forces beneath Europa's frozen shell can cause large blocks of
ice to overturn and
melt, bringing vast pockets of water, sometimes holding as
much liquid as all of the Great Lakes combined, to within several kilometers of the moon's icy surface.
That is bad news, because warm water
melts ice much faster than warm air.
«In recent years Arctic pack
ice has formed progressively later,
melted earlier, and lost
much of its older and thicker multi-year component,» says Anthony Fischbach of the US Geological Survey (USGS) and one of the research team.
Ullman said the level of CO2 that helped trigger the
melting of the Laurentide
ice sheet was near the top of pre-industrial measurements — though
much less than it is today.
Better estimates of Pliocene sea levels will help geologists know how
much of the
ice sheets
melted during that balmy era, Dowsett says, which may give us a glimpse of our own climate future.
«The
ice cover becomes less and less resilient, and it doesn't take as
much to
melt it as it used to,» Meier said.
Not only is Greenland's
melting ice sheet adding huge amounts of water to the oceans, it could also be unleashing 400,000 metric tons of phosphorus every year — as
much as the mighty Mississippi River releases into the Gulf of Mexico, according to a new study.
«Warming greater than 2 degrees Celsius above 19th - century levels is projected to be disruptive, reducing global agricultural productivity, causing widespread loss of biodiversity and — if sustained over centuries —
melting much of the Greenland
ice sheet with ensuing rise in sea levels of several meters,» the AGU declares in its first statement in four years on «Human Impacts on Climate.»
In the San Francisco Bay area, sea level rise alone could inundate an area of between 50 and 410 square kilometres by 2100, depending both on how
much action is taken to limit further global warming and how fast the polar
ice sheets
melt.
If the water remained in the channel, the water would eventually cool to a point where it was not
melting much ice, but the channels allow the water to flow out to the open ocean and warmer water to flow in, again
melting the
ice shelf from beneath.
The same hotspot in Earth's mantle that feeds Iceland's active volcanoes has been playing a trick on the scientists who are trying to measure how
much ice is
melting on nearby Greenland.
NSIDC scientists said there was a lot of thin
ice at the beginning of the
melt season, because thinner
ice does not take as
much energy to
melt away, this may have also contributed to this year's low minimum extent.
Previous studies have attributed those undersea channels — which measure between 1 and 2 km wide and extend up into the
ice shelf as
much as 400 meters — solely to the
melting action of seawater.
Last Friday afternoon, on a conference call hosted by the National Research Council to present a recent report on the Arctic region, Stephanie Pfirman, an environmental science professor at Barnard College, said Arctic
ice coverage is shrinking and that thicker sea
ice blocks, which anchor
much of the landscape, are rapidly
melting.
When the planet's big
ice sheets collapsed at the end of the last
ice age, their
melting caused global sea levels to rise as
much as 100 meters in roughly 10,000 years, which is fast in geological time, Mann noted.
«If
ice caps and glaciers were to continue to crack and break into pieces, [the amount of] their surface area that is exposed to air would be significantly increased, which could lead to accelerated
melting and
much - reduced coverage area on the Earth,» Buehler said in a statement.
«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.
Shepherd said, though, that there still is still a lot of uncertainty about how
much additional
melt in some locations of the Greenland
ice sheet will actually be lost to the ocean.
The first comprehensive survey of all Antarctic
ice shelves discovered that basal
melt, or
ice dissolving from underneath, accounted for 55 percent of shelf loss from 2003 to 2008 — a rate
much higher than previously thought.
A relatively small amount of
melting over a few decades, the authors say, will inexorably lead to the destabilization of the entire
ice sheet and the rise of global sea levels by as
much as 3 meters.
To determine how
much ice would
melt around
ice - free areas over the next 80 years as the climate warms, Ms Lee worked alongside colleagues from UQ, CSIRO, the Australian Antarctic Division and the British Antarctic Survey.
It takes a while for that
much ice to
melt, of course.