While
exposed water ice would not be stable at the surface of Ceres at its relatively close distance to the Sun, water and ammonia do appear to be bound up in crustal minerals on the asteroid's surface.
Last year the Herschel Space Observatory detected wisps of water vapor around the dwarf planet, and since its arrival at Ceres, Dawn has imaged oodles of highly reflective bright spots on the Cereian surface that may be sites of
exposed water ice.
Alice also documented a surprising lack of
exposed water ice on the comet's surface and identified an extremely volatile, unexpected gas in the comet's atmosphere — molecular oxygen.
[2] It has been suggested that the highly reflective material in the spots on Ceres might be freshly
exposed water ice or hydrated magnesium sulphates.
Not exact matches
Hints of the special phase, called superionic
ice, appeared in
water ice exposed to high pressures and temperatures, researchers report February 5 in Nature Physics.
Any parts of the bed this low are easily
exposed to ocean
water, allowing the
ice sheet to weaken from below as the ocean
water warms.
Now, researchers have
exposed a more accessible analog for extraterrestrial life habitats: microscopic pockets of salt
water in the Arctic Ocean's winter
ice.
Things get otherworldly at the rear of the lab, where the researchers create temporary caves of dirty blue and black
ice by blasting through an
exposed ice wall with hot
water for at least 24 hours.
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.
The deposits are
exposed in cross section as relatively pure
water ice, capped by a layer one to two yards (or meters) thick of
ice - cemented rock and dust.
At some of them, the
exposed deposit of
water ice is more than 100 yards, or meter, thick.
Impacts
exposing subsurface
ice deposits and generating hydrothermal activity are one possible explanation for the bright spots and Herschel's
water vapor; «cryovolcanoes» that erupt volatiles such as
water rather than rock are another.
The melting of sea
ice is
exposing more ocean
waters in the Arctic, but they are showing a limited ability to dispose of CO2, according to a new study
Worse still, in places like west Antarctica,
ice sheets rest on land that is below sea level, and so could be
exposed directly to warm
water.
«The sea
ice cap, which used to be a solid sheet of
ice, now is fragmented into smaller floes that are more
exposed to warm ocean
waters.
However, on January 12 in Science, Dundas and colleagues reported finding eight slopes where layers of
water ice were
exposed at shallow depths (SN Online: 1/11/18).
Warmer temperatures melt the Arctic
ice and
exposes water, which absorbs more sunlight than
ice.
As climate change causes sea
ice to shrink — and new
waters open to human exploration — this single - tusked cetacean will likely be
exposed to new noises and new threats.
These blooms, which turn the sea from deep blue to lush green, begin sometime in November in a large polynya (an opening in the
ice) in the Ross Sea when the liquid
water is
exposed to sunlight.
As a result of atmospheric patterns that both warmed the air and reduced cloud cover as well as increased residual heat in newly
exposed ocean
waters, such melting helped open the fabled Northwest Passage for the first time [see photo] this summer and presaged tough times for polar bears and other Arctic animals that rely on sea
ice to survive, according to the U.S. Geological Survey.
And, worryingly, the research suggests that as these glaciers melt and retreat backward, the shape of the seabed will continue to
expose many of them to warm ocean
water for hundreds of miles as the
ice moves inland.
The researchers had expected the ocean to play a bigger role in eroding away the coastline, as it has elsewhere — especially as climate change is causing more Arctic sea
ice to melt away, leaving the surface of the
water exposed.
If they begin to melt, however — particularly as they're
exposed to warmer ocean
water — the shelves become thinner and the grounding line begins to retreat backward, causing the glacier to become less stable and making the
ice shelf more likely to break.
Because so much
water was stored on land as
ice sheets, sea levels were likely 120 meters lower than today,
exposing the bottom of what is now the English Channel.
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.
This creates thicker, longer - lasting
ice, while
exposing surrounding
water and thin
ice to the blistering cold winds that cause more
ice growth.
With Arctic
ice retreating more and more as local summers heat up,
exposing ever more cold northern
waters to warming sunshine — along with a host of other regional changes — it remains to be seen exactly how sensitive global climate really is.
This is an important discovery since it
exposed that
water ice was considerably more widespread than what was hypothesised.
Scientists already know that receding sea
ice allows solar energy to warm
exposed water rather than reflect back into space, but blooms of algae could make matters even worse.
Because the temperature of Ceres is relatively warm (between -93 ℃ and -33 ℃),
water -
ice exposed at the surface would rapidly convert into a gas in such a low - pressure environment.
So the discovered traces of
water -
ice suggest some underground
ice was recently
exposed and that there must be some mechanism to explain how the surface was disturbed in this way.
During glaciation,
water was taken from the oceans to form the
ice at high latitudes, thus global sea level drops by about 120 meters,
exposing the continental shelves and forming land - bridges between land - masses for animals to migrate.
But when sea
ice melts, it
exposes the darker surface of the underlying
water, which absorbs solar energy.
The underlying logic is sound: as sea
ice melts, it
exposes darker ocean
water, which absorbs more of the sun's heat, causing the
water temperatures to increase.
The thickness of the remaining, multi-year
ice, along with its geographic location, will make it more difficult to melt than the
ice that was spread across the Arctic, and
exposed to Pacific and Atlantic ocean currents, along with runoff from fresh
water rivers.
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.»
At this pit on Mars, the steep slope at the northern edge (toward the top of the image)
exposes a cross-section of a thick sheet of underground
water 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.
Rock salt and other salt - based
ice melters contain sodium chloride or potassium chloride which can heat up to 175 degrees when
exposed to
water,
ice, and low temperatures.
Once the
water is completely frozen, peel back the paper from the top of the cup to
expose a half - inch to 1 inch of
ice.
Some pet parents casually mention dropping
ice cubes into their pet's
water bowl, while others create urgent - sounding blog posts that seem to suggest we are killing our cats by
exposing them to a couple
ice chips every now and then.
Glacial
ice that floats in the
water is only 10 percent
exposed, the remaining 90 percent is under
water.
The physical processes by which energy might be added into the glacier material include: (A) convection between the glacier surfaces and local surrounding atmosphere and
water, (B) direct radiation onto the
exposed surfaces of the material, (C) addition of material that is at a temperature higher than the melting temperature onto the top of the glacier (rain, say), (D) Sublimation of the
ice directly into the atmosphere, and (E) conduction into the material from the contact areas between the glacier and surrounding solid material.
The strong winds from the south can push the
ice further north into the Central Arctic,
exposing the open
water and releasing heat to the atmosphere from the ocean.»
What a great gift to have a reliably
ice - free Northwest passage for 2 - 3 months per year (it can't be much more than that, what with long sunless winters and efficient IR emissive cooling from
exposed water).
(He was using a board to test the edge of a «lead» in the
ice exposing water that is 29 degrees Fahrenheit and about 14,000 feet deep.)
The smaller the lid gets — because warmer
water is eating away at its edges and its underside — the more that warmer
water is
exposed to the local air mass, the less that air is cooled by contact with
ice.
The
exposed open
water caused by the wind divergence may absorb some additional sunlight and melt more
ice than usual over the next few weeks (temperature - albedo feedback)[related NASA animation], but given that the sun is well on its way to setting for the winter, I think this effect will be fairly minimal.
[The move] is aimed at avoiding big ecological disruptions as the expanding summer retreats of sea
ice on the Arctic Ocean
expose virgin
waters.
My take on this is that in August the Arctic Ocean's
ice carapace reaches its minimum and consequently the maximum surface area of the coldest sea
water on the planet is
exposed to the atmosphere.