The images show the extent of Greenland
surface ice melt on July 8 (left) and July 12 (right).
In spite of the headline, the press release itself went on to explain how the «unprecedented» extent of
surface ice melt wasn't, in fact, unprecedented.
And as a bonus for Gorites, it would dramatically reduce
surface ice melt.
AS THE Earth warms, so
its surface ice melts into the sea: true in the past, and true in the future.
«There are already places in the Andes, for instance, where records of the last 30 to 40 years have disappeared because of
surface ice melting,» Rignot says.
The highs tend to enhance the flow of warm, moist air over Greenland, contributing to increased extreme heat events and
surface ice melting, according to the study.
«Just when
the surface ice melted in the lab, he measured a large flux of carbon and methane.
As when
surface ice melts, well up bobs ice below to continue the melt.
On July 12, a series of unusually warm ridges of air, or heat domes, that have been centred over Greenland since May, contributed to 97 % of
the surface ice melting.
Not exact matches
The study suggests that up until 1997, whenever the
ice caps and glaciers
melted, the runoff would be filtered through a layer of older snow called the «firn» and trickle down to the
ice surface, where it would freeze again, allowing the glaciers and
ice caps to grow each winter.
It looks gorgeous, and, due to the larger
surface area of the
ice, it
melts very slowly, so your punch won't get too diluted.
Salt lowers the
melting point of
ice (and we might investigate this process later on), but by doing so it means that the
surface of the can is actually below freezing point.
It can be used as a concrete safe
ice melt because it «lingers» on the
surface it's applied to.
Scientists first thought this water was
melting from
surface ice, but that interpretation is less likely for the slopes near the equator, where the
surface is probably too warm for
ice.
Warm mountain winds are causing extensive winter
melting on the
surface of the Larsen C
ice shelf, which could contribute to its breakup
And when they land on Greenland's snow and
ice, their ability to absorb heat from sunlight increases
surface melting.
The thermodynamic model developed by VTT Technical Research Centre of Finland research scientists shows that under certain conditions
ice warms and
melts when an item of material slides across its
surface.
Under certain conditions, the warm water of the lower layer can reach the
surface and
melt the
ice.
Higher precipitation levels in the region and
melting ice would decouple the
surface from the deeper water layers.
The Greenland
ice sheet occupies about 82 % of the
surface of Greenland, and if
melted would cause sea levels to rise by 7.2 metres.
In permafrost,
ice holds up the soil; when the
ice melts, the land
surface slumps, creating features known as thermokarst failures.
On Pluto, a slurry of nitrogen and water
ice melted by subsurface heat stands in for lava, the team suggests, freezing solid once it is exposed at the
surface.
When the researchers took density of snow into account, they found that
ice shelves lost about five times more
ice by submarine
melting than they gained from new
surface snowpack.
That translates to a depth of roughly 1,492 meters below the
surface of Greenland and is marked by its own isotopic changes, thanks to all that
melting ice.
This allowed them to calculate the redistribution of mass on Earth's
surface due to the
melting of the Greenland and Antarctic
ice sheets and mountain glaciers, and model the shift in Earth's axis.
increasing air temperatures on the Antarctic Peninsula, which can enhance
surface melting of
ice shelves,
«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.
«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.»
«Everywhere the
ice surface was
melting I could see a mauve colour,» he says.
Using computer modeling to interpret images from NASA's Galileo satellite, Pappalardo and Barr demonstrated that acnelike markings on Europa's
surface are probably bits of
ice containing minerals such as chloride salts and sulfuric acid, which lower the
melting point so the material can rise from deep below.
But last year, Arrigo and his team noted a proliferation of pools of water, known as
melt ponds, on the
surface of the Chukchi Sea
ice, which were also a few meters thinner than in past years.
Untersee is a good model for Mars, he says, because it is supplied by subglacial
melt — water that accumulates at the bottom of an
ice pile — rather than from
surface melting, which does not occur on Mars.
As many
surface melt - water lakes form each summer around the Greenland
ice sheet, the possibility exists that similar subglacial lakes may be found elsewhere in Greenland.
The researchers propose that, unlike in Antarctica where
surface temperatures remain below freezing all year round, the newly discovered lakes are most likely fed by
melting surface water draining through cracks in the
ice.
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.
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.
Quantitative analysis has evidenced the acceleration system of
melting ice: dark water
surfaces absorb more heat than white
ice surfaces, thus
melting ice and making more water
surfaces in the Arctic Ocean.
Thinner
ice means a darker
surface, which increases the region's capacity to store heat and thus enables more
melting.
But the water's source — whether
melting ice, rainfall, or groundwater — and its duration on the
surface are still open questions.
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.
The data allowed them to calculate the redistribution of mass on Earth's
surface due to the
melting of the Greenland and Antarctic
ice sheets and mountain glaciers, and the resulting rise in sea level.
Analyzing the data from 1979 to 2014, the researchers found the solar heat input through open water
surfaces correlated well with
ice melt volume, suggesting heat input is a major causative factor of
melting ice.
David Ullman, a postdoctoral researcher at Oregon State University and lead author on the study, said there are two mechanisms through which
ice sheets diminish — dynamically, from the jettisoning of icebergs at the fringes, or by a negative «
surface mass balance,» which compares the amount of snow accumulation relative to
melting.
The
ice sheet got hammered by
surface melt, and that's what drove final deglaciation.»
This created hot springs that flowed to the
surface and
melted ice there.
As the sea
ice melts, its white reflective
surface is replaced by a relatively dark ocean
surface.
The two main forces that conspire to destroy Earth's massive polar
ice sheets are heat, which
melts their
surfaces via sunlight and warm air, and gravity, which drives glaciers to slide to the sea.
In 2002, NASA's Odyssey orbiter detected evidence of
ice just beneath the
surface of the Martian north pole, raising the possibility that during a warm spell liquid water could
melt out — a likely requirement for life.
In Iceland, the Grimsvotn volcano, buried miles beneath the
ice sheet,
melts the
ice cap above it in the same way that the rising plumes might
melt Europa's shell, causing the
surface of the Icelandic
ice sheet to cave in.
Warm air and
surface water are
melting the summer polar
ice cap.