Not exact matches
Many scientists think these permanently shadowed
regions, such as the floors on impact craters
in the Moon's polar
regions, could hold large deposits or
water ice.
The new study «demonstrates that climate change can remobilize POPs stored
in water, snow,
ice and presumably soils — and that this process is already occurring
in the Arctic
region,» he wrote
in an essay accompanying the new study.
Forming
in the system's colder outer
regions, where volatile compounds such as
water and carbon dioxide freeze out, makes it possible that the planets incorporated those
ices and carried them along to a warmer place where they could melt, evaporate, and become oceans and atmospheres.
Completed
in 1980 but operational before then, the VLA was behind the discoveries of
water ice on Mercury; the complex
region surrounding Sagittarius A *, the black hole at the core of the Milky Way galaxy; and it helped astronomers identify a distant galaxy already pumping out stars less than a billion years after the big bang.
Higher precipitation levels
in the
region and melting
ice would decouple the surface from the deeper
water layers.
The fall of the temperature of the sea
water is sometimes a sign of the proximity of
ice, although
in regions where there is an intermixture of cold and warm currents going on, as at the junction of the Labrador Current and the Gulf Stream, the temperature of the sea has been known to rise as the
ice is approached.
Water vapor and clouds may play a role The Arctic's summer
ice cover hit a record low
in 2007, when it dipped about 40 percent below the average
ice cover recorded since 1979, when scientists began monitoring the
region with satellites.
These particles can build up electric charges faster than the soil can dissipate them and may cause sparking, particularly
in the polar cold of permanently shadowed
regions — unique lunar sites as cold as minus 240 degrees Celsius and known to contain
water ice.
Next summer is expected to be the third
in a row with completely
ice - free
waters above the Arctic Circle, and tourism
in the once - remote
region is thriving.
While that
water could initially come from Earth, it could later come from
water ice frozen on asteroids,
in shadowed
regions of the moon's surface, from possible sources on Mars» two moons, or from Mars itself.
The scientists were able to use a test scenario
in the Greenland Sea to demonstrate that ALES + returns
water levels for
ice - covered and open ocean
regions which are significantly more precise than the results of previous evaluation methods.
A cloud front can be seen
in the lower left, and dark areas indicate
regions of open
water between sea
ice formations.
A possible cause for the accelerated Arctic warming is the melting of the
region's sea
ice, which reduces the icy, bright area that can reflect sunlight back out into space, resulting
in more solar radiation being absorbed by the dark Arctic
waters.
This line marks a deep ocean channel that remained
water - filled even during past
ice ages, when sea levels saw channels between other islands
in the
region dry out.
«A lot of what we are seeing right now
in the coastal
regions is that warming ocean
waters are melting Antarctica's glaciers and
ice shelves, but this process may just be the beginning,» Shevenell said.
Invasive species are entering the
region with or without shipping, says Ted Scambos of the National Snow and
Ice Data Center
in Colorado; warming of the Arctic Ocean's surface temperatures has already increased mixing with foreign
waters and all the microbes they contain.
«This is the first - ever such survey
in the Northwest Passage, and we were surprised to find this much thick
ice in the
region in late winter, despite the fact that there is more and more open
water in recent years during late summer,» says Haas.
«Unique diamond impurities indicate
water deep
in Earth's mantle: Scientific analysis of diamond impurities — known as inclusions — reveal naturally forming
ice crystals and point to
water - rich
regions deep below the Earth's crust.»
First of all, less sea
ice is forming
in the
region, and secondly, oceanographic recordings from the continental shelf break confirm that the warm
water masses are already moving closer and closer to the
ice shelf
in pulses,» says Dr Hartmut Hellmer, an oceanographer at the AWI and first author of the study.
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.
To assess whether liquid
water flowed over the
region during the heat spells Mars experiences every 50,000 years, an onboard microscope will examine cracks
in the subsurface
ice that should form during cold times.
According to the geochemist, comets originate
in the cool outer
regions of the solar system where volatile
water and carbon compounds condensed into
ice.
That includes mixedphase clouds, which occur
in polar
regions and combine supercooled
water with
ice.
As the paper suggests, one could be the evaporation of surface
waters that have become exposed because of sea
ice loss
in the
region, he added.
«The upper haze is so optically pretty thick that it is only
in the stormy
regions where the haze is penetrated by powerful updrafts that you can see evidence for the ammonia
ice and the
water ice.
The data from Keck Observatory shows that peroxide is widespread across much of the surface of Europa, and the highest concentrations are reached
in regions where Europa's
ice is nearly pure
water with very little sulfur contamination.
Scientists think that
in the «heart»
region of Pluto (otherwise known as Sputnik Planum),
water ice bedrock might be hidden underneath a thick blanket of other
ices made of methane, nitrogen and carbon monoxide.
The new results show that atmospheric
water in the near - polar
region was enriched by a factor of seven relative to Earth's ocean
water, implying that
water in Mars» permanent
ice caps is enriched by 8-fold.
The team was especially interested
in regions near the north and south poles, because the polar
ice caps are the planet's largest known reservoir of
water.
Reference: «New Evidence for Surface
Water Ice in Small - Scale Cold Traps and
in Three Large Craters at the North Polar
Region of Mercury from the Mercury Laser Altimeter,» Ariel N. Deutsch, Gregory A. Neumann & James W. Head, 2017 Sept. 14, Geophysical Research Letters [http://onlinelibrary.wiley.com/doi/10.1002/2017GL074723/full].
«Soil thickness,
ice presence and depth, atmospheric circulation, and sunshine can explain the current difference
in the amount of
water in the soil of different
regions,» as IFL Science reports.
Collapsing
ice shelves and melting sea
ice leaves more open
water in the Earth's polar
regions (photo a
in earlier figure).
Are you saying that ocean circulation patterns
in the Northern Hemisphere do not reach Antarctic
regions where
ice is more
in the
water?
While it is often occurring
in remote
regions, ongoing change with the cryosphere has impacts on people all around the world: sea level rise affects coastlines globally, billions of people rely on
water from snowpack, and the diminishing sea
ice that covers the Arctic Ocean plays a significant role
in Earth's climate and weather patterns.
The surface is composed of three major types of terrain: bright, rough
regions that are similar to Xanadu Regio, dark
regions that are rich
in water ice, and dark
regions that are covered by fields of dunes.
But they do at least have certain basic physical principles
in their cloud representations — clouds over
ice have less albedo effect than clouds over
water, you don't get high clouds
in regions of subsidence, stable boundary layers lead to marine stratus, etc..
On March 21, 2012, the MESSENGER team also revealed new supporting evidence that many permanently shadowed craters
in Mercury's polar
regions may harbor
water ice insulated with a thin layer of soil or dust, or some other radar - reflecting volatile substance such as sulfur.
Warm
waters have been eating away at
ice from below
in this
region, and once grounding lines retreat far enough inland, entire glaciers can become unstable and collapse.
This is the external or internal use of
water in any form (i.e.,
ice, steam, or
water) with various temperatures, pressures, and durations to treat multiple
regions of the body.
When the Arctic sea
ice goes the increase
in water vapour
in the Arctic
region will accelerate the Greenland melt.
If the NAO were driving an ocean current that contains higher SST's and more saline surface
water into the Arctic
region, I suspect it would be a possible correlation that salinity may be playing a part
in the Arctic
ice loss.
It is possible the Arctic
ice melt could also be related to ocean currents carrying highly saline
water caused by the recent increased SSTs
in the temperate oceans between 1985 and 2005 to the
region.
Over all, open
water has spread
in the Arctic this summer nearly as much as it did last summer, when polar experts said the
ice cap shrank far more than had been measured since satellites started scanning the
region 30 years ago — and probably more than it had shrunk
in a century or more.
I've been to the Arctic three times for the newspaper since 2003 — visiting the North Slope, North Pole, and Greenland to examine what mix of human and natural forces is driving the warming and
ice retreats and the implications of having increasing amounts of open
water in summers
in a
region increasingly seen as a resource trove and shortcut for shipping.
This would seem to suggest that if the volume of
ice melt is as great as suspected, that there had to be a greater salinity
in the
region that was mixing with the melt
water to reduce the expanse and depth of the brackish
region.
In many regions, changing precipitation or melting snow and ice are altering hydrological systems, affecting water resources in terms of quantity and quality (medium confidence
In many
regions, changing precipitation or melting snow and
ice are altering hydrological systems, affecting
water resources
in terms of quantity and quality (medium confidence
in terms of quantity and quality (medium confidence).
Added to this the seas
in these
regions recede as the gravitational pull of the
ice is no longer present, leading to the redistribution of this
water to the equator.
Last summer's record loss of
ice was due to a combination of natural cycle and global warming factors: «more greenhouse gases, an unusual wind pattern, and warming of the ocean
water in regions with reduced sea
ice.»
In the
region above the temperature maximum, Atlantic
Water heat can go upward and affect the sea
ice.
Historically, there had not been enough open
water for polar bears
in this
region to swim the long distances we observed
in these recent summers of extreme sea
ice retreat.»