Only four days before, just 40 percent of
the surface ice layer was thawing.
«The Greenland ice sheet, which is up to 3000 + metres thick, is not «melting away», did not «melt in four days», it is not «melting fast», and Greenland did not «lose 97 per cent of
its surface ice layer».»
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.
Spoon the
ice cream into the dish in an even
layer and smooth up the
surface with the back of a spoon.
Spread a thin
layer across the
surface of the green
ice cream, smoothing to cover it completely.
«The
surface layer between
ice and liquid is very complicated,» he says.
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.
These
ice deposits would likely require a thin insulating blanket, perhaps a
layer of fine - grained
surface material, or regolith, to keep it from sublimating away.
Scientists aren't sure if it has a rocky
surface or one that's buried beneath thick
layers of gas and
ice.
He argues that such
surfaces can easily form a new
layer of
ice or even frost flowers — rare (and gorgeous)
ice crystals that grow upward from the sea.
Using the Shallow Radar instrument aboard NASA's Mars Reconnaissance Orbiter, Holt was able to peek beneath the
ice's
surface for clues; in particular, the radar could pick out differences in electrical reflectivity between overlying
layers, showing how the
ice built up over time.
SLIPS's thin
layer of liquid lubricant allows liquids to flow easily over the
surface, much as a thin
layer of water in an
ice rink helps an
ice skater glide.
Finding a
layer of ash in the
ice wouldn't be surprising: the West Antarctic Ice Sheet straddles a broad continental rift that is known to harbor volcanoes, some of them exposed on the surface and others sealed under i
ice wouldn't be surprising: the West Antarctic
Ice Sheet straddles a broad continental rift that is known to harbor volcanoes, some of them exposed on the surface and others sealed under i
Ice Sheet straddles a broad continental rift that is known to harbor volcanoes, some of them exposed on the
surface and others sealed under
iceice.
The new
ice - scarp studies confirm indications from fresh - crater and neutron - spectrometer observations that a
layer rich in water
ice begins within just one or two yards of the
surface in some areas.
Fissures and fractures around Tombaugh Regio and other parts of the planet suggested a subsurface
layer of watery slush might be slowly solidifying, breaking up the
surface as it expands like
ice cubes in a freezer — but other, drier possibilities could also explain such cracks.
The glacier
ice found by the team, which came from a
layer that began just 50 centimetres below the
surface, was dated by analysing the relative abundances of isotopes of argon in a thin
layer of overlying volcanic ash.
The drought that is devastating California and much of the West has dried the region so much that 240 gigatons worth of
surface and groundwater have been lost, roughly the equivalent to a 3.9 - inch
layer of water over the entire West, or the annual loss of mass from the Greenland
Ice Sheet, according to the study.
Bright, streaky material visible underneath many of the craters all but proves that Phoebe's dusky
surface is in fact a thin
layer on top of a mother lode of
ice, Mitchell says.
Using spectral readings from telescopes at the Keck Observatory in Hawaii, Hand has found high levels of oxidative chemicals such as sulfate, oxygen, sulfur dioxide and hydrogen peroxide on Europa's
surface, which are produced as ionizing radiation from Jupiter scours it, splitting apart water molecules and sulfur compounds in the uppermost
layers of its
ice.
The top
layer is superhydrophobic, preventing freezing rain from forming
ice on the
surface.
They also looked at whether craters made by the comets hitting the
surface could excavate enough nitrogen — but that would require a very deep
layer of nitrogen
ice at the
surface, which is not proven.
New research shows how a
layer of water on the
surface of
ice — even at temperatures well below freezing — can influence everything from the slipperiness of a skating rink to the electrification of thunderclouds
But the bottoms - up
ice formation could make finding that old
ice harder, since the new
layer of
ice scrambles the older
layers of
ice above it, or it could make it easier, because the older
ice will be closer to the
surface of the
ice sheet.
That base
layer can warp and lift the
ice above it, which is formed by snow deposited on the
ice sheet's
surface.
Researchers were surprised to find a 7,700 - square - mile piece (about the size of Wales) missing, but they theorized that it had moved over warmer
ice layers until it collided with another plate and was forced beneath the
surface, out of view.
To melt only the
ice layer immediately in contact with the
surface, he has developed a way of pulsing electric current into the heater in 1 - millisecond bursts.
The craft is designed to dig into the cementlike
layer of
ice that researchers believe lies buried a few inches below the
surface in the planet's polar regions, scanning for signs of past liquid water and organic compounds, the carbon - rich molecules that make life on Earth possible.
«In the past this extensive warmth was well isolated from the
surface layers and
ice by a fresh cold
layer... Our moorings demonstrated that this
layer disappeared in 2013 - 14 and 2014 - 15 winters, which has never been observed of the Arctic Ocean before,» said Polyakov.
The instrument sends down radar waves, which reflect off of the
ice surface,
layers inside the
ice sheet and bedrock back to the instrument, giving researchers a three - dimensional view.
The P - 3 Orion, based at NASA's Wallops Flight Facility in Virginia, will carry IceBridge's most comprehensive instrument suite: a scanning laser altimeter that measures
surface elevation, three types of radar systems to study
ice layers and the bedrock underneath the
ice sheet, a high - resolution camera to create color maps of polar
ice, and infrared cameras to measure
surface temperatures of sea and land
ice.
Very little happening in summer itself (as expected) as the melting
ice surface and heat sensible heat gain in the mixed
layer limit the
surface air temperature change.
The reason for that, they suggest, is that instead of landing directly on the
surface, ejecta from Lyot landed on a thick
layer of
ice, which prevented it from gouging the
surface beneath the
ice.
Bacteria, however, have remained Earth's most successful form of life — found miles deep below as well as within and on
surface rock, within and beneath the oceans and polar
ice, floating in the air, and within as well as on Homo sapiens sapiens; and some Arctic thermophiles apparently even have life - cycle hibernation periods of up to a 100 million years while waiting for warmer conditions underneath increasing
layers of sea sediments (Lewis Dartnell, New Scientist, September 20, 2010; and Hubert et al, 2010).
«The reason for the
layering is that global warming in parts of Antarctica is causing land - based
ice to melt, adding massive amounts of freshwater to the ocean
surface,» said ARC Centre of Excellence for Climate System Science researcher Prof Matthew England an author of the paper.
The research published in Nature Communications found that in the past, when ocean temperatures around Antarctica became more
layered - with a warm
layer of water below a cold
surface layer -
ice sheets and glaciers melted much faster than when the cool and warm
layers mixed more easily.
Weinberger designed the observations to be able to detect large water
ice grains in the
surface layer of the disk.
The distribution of the flow types varies with latitude — and the researchers think this means different
surface layers of the asteroid contain different amounts of
ice.
Pritchard et al. used a combination of satellite laser altimetry and modelling of the
surface firn
layer to show
ice - shelf thinning around Antarctica as a result of increased basal melt.
The researchers found a
layer of smooth
ice had grown on the graphene, not the usual puckered
layers of
ice seen on water friendly or hydrophilic
surfaces.
The Danish Meteorological Institute reported that although it's only April, nearly 12 percent of the
ice sheet's
surface is covered with a
layer of meltwater of a depth of at least a millimeter.
At sites across the midsection of Mars, scientists have found
layers of water
ice buried mere feet beneath the red planet's
surface.
Impact craters at many latitudes sometimes expose thin
ice layers a foot or so beneath Mars»
surface.132 «At polar latitudes, as much as 50 percent of the upper meter of soil may be [water]
ice.»
When an icy impact occurred, the impactor's kinetic energy became heat energy, instantly melted some
ice, gouged out a crater, and kicked up into Mars» thin atmosphere large amounts of debris mixed with water (liquid,
ice crystals, and vapor)-- and complex organic molecules that obviously came recently from life.127 Then, the dirt and salt - water mixture settled back to the
surface in vast
layers of thin sheets — strata — especially around the crater.
Compositional data also show that the
surface of Piri Planitia is more enriched in water
ice (shown in false colour as blue) than the higher plateaus, which may indicate that Piri Planitia's
surface is made of water
ice bedrock, just beneath a
layer of retreating methane
ice.
They suspect that the methane
ice - rich
surface on Pluto may be sublimating away into the atmosphere, exposing a
layer of water -
ice underneath.
As this water moves through rocks, it dissolves salt compounds and pushes through fractures in the overlying
ice to form reservoirs closer the moon's
surface, where it is expelled into space when the outermost
layer of the crust cracks open and the resulting depressurization of these reservoirs causes water vapor and
ice particles to shoot out in the observed plumes.
A key characteristic of the locations where CO2
ice condenses is that there is always a permafrost
layer composed of water
ice - cemented grains a few centimeters below the
surface.
Using a spatula spread a
layer of maple
icing over the
surface.
The outer
layer of Safe Paw granules liquefies on contact with
ice and begins to penetrate and break up the
surface.