During aphelion
water ice clouds form in the atmosphere, interacting with the dust particles and affecting the temperature of the planet.
Interannual variability of
water ice clouds over major martian volcanoes observed by MOC J. L. Benson, P. B. James, B. A. Cantor and R. Remigio Icarus 184, 365 — 371, doi: 10.1016 / j.icarus.2006.03.014, October 2006.
This composite of 7.5 km (4.7 mi) per pixel daily global images, acquired by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC), shows
water ice clouds over and to the east (right) of the Mars Exploration Rover (MER - B), Opportunity, landing site in Meridiani Planum.
Here, bluish - white
water ice clouds hang above the Tharsis volcanoes.
Not exact matches
Newly formed
ice crystals fall earthward, and the energy released in their transition from liquid to solid evaporates nearby
water drops, leaving a hole in the
cloud.
Each snow crystal forms when
water vapor in the
clouds condenses into
ice.
The extremely low temperatures and rapid freezing were crucial to forming cubic
ice, Wyslouzil said: «Since liquid
water drops in high - altitude
clouds are typically supercooled, there is a good chance for cubic
ice to form there.»
«This imaging was part of an experiment checking the opacity of the atmosphere at night in Curiosity's location on Mars, where
water -
ice clouds and hazes develop during this season,» said camera team member Mark Lemmon of Texas A&M University, College Station.
Researchers created
ice crystals with a near - perfect cubic arrangement of
water molecules, in order to better understand how high - altitude
ice clouds interact with sunlight and the atmosphere.
Many
clouds at mid-latitudes make rain by freezing
water into
ice crystals (which fall from the
cloud then melt before they hit the ground), rather than by coalescing warm
water droplets together.
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.
Among the findings is strong evidence for the existence of
clouds of
water or
water ice, the first such
clouds detected outside of our solar system.
The conclusion that limiting CO2 below 450 ppm will prevent warming beyond two degrees C is based on a conservative definition of climate sensitivity that considers only the so - called fast feedbacks in the climate system, such as changes in
clouds,
water vapor and melting sea
ice.
Effects of plasma channels on
ice formation or precipitation processes could not be proved in typical storm
clouds, where
ice crystals and subcooled
water droplets coexist.
A
cloud front can be seen in the lower left, and dark areas indicate regions of open
water between sea
ice formations.
«Our analysis confirmed that the Planck Response plays a dominant role in restoring global temperature stability, but to our surprise we found that it tends to be overwhelmed locally by heat - trapping positive energy feedbacks related to changes in
clouds,
water vapor, and snow and
ice,» Brown said.
Given what scientists know about the Red Planet's atmosphere, these
clouds likely consist of either carbon dioxide or
water - based
ice crystals.
By analyzing this data over the following six months, the researchers found that
clouds that grew at the lowest temperatures required extremely high relative humidity in order for
water vapor to form an
ice crystal around a dust particle.
Hence, the
clouds that form at colder temperatures — if any form at all — contain much less suspended
water in the form of
ice crystals, the starting sites for snow crystal formation.
Once those silver iodide particles make their way into a ripe
cloud, they collide with drops of supercooled
water and form
ice; the
ice then falls to the ground, melting along the way.
Even models that correctly capture
cloud behavior may fail to fully account for other climate feedbacks from factors like changing snow and sea
ice cover, atmospheric
water vapor content, and temperature.
«A sort of grand problem in Earth science is to understand the
water cycle — evaporation from the ocean,
clouds, rain, the formation of
ice, the runoff from the land back into the sea,» said Eric Lindstrom, Aquarius program scientist at NASA.
In addition, he says, since CFCs are not particularly soluble in
water, they would not be present in
cloud - born
ice particles in very high concentrations, so the mechanism Lu and Sanche propose would not dissociate enough CFCs to have a big impact on ozone levels.
The coldest
clouds are full of
ice; the warmest are full of
water.
The mountains are made primarily of rock - hard
water ice; the dunes are most likely
ice granules coated with hydrocarbons; volcanoes probably belch methane and ammonia, and methane fills the lakes, evaporates to form
clouds, and rains back down to carve out river channels.
«Lightning is caused by charge separation within
clouds, and to maximize charge separation, you have to loft more
water vapor and heavy
ice particles into the atmosphere,» he said.
«When carbon dioxide concentrations and temperatures rise, then mixed - phase
clouds will increase their liquid
water content,» said Ivy Tan, a PhD candidate at Yale University who led the research, which investigated common
clouds that contain both
ice and
water.
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.
They pointed a variety of infrared telescopes at interstellar dust
clouds and discovered dips at specific frequencies corresponding to molecules including methanol, ammonia, and
water ice.
That includes mixedphase
clouds, which occur in polar regions and combine supercooled
water with
ice.
The «factors» are natural phenomena such as
water vapor,
clouds, sea
ice, dust and vegetation — all of which exert varying pulls on the climate.
That rover has stayed close to one spot for the last nine months, where among other observations, it spotted the first
water -
ice clouds identified from the surface of Mars.
In the latter scenario,
water ice would make up 22 percent of the
cloud head and ammonia
ice 55 percent.
The key finding:
cloud particles at the top of the great storm are composed of a mix of three substances:
water ice, ammonia
ice, and an uncertain third constituent that is possibly ammonium hydrosulfide.
The interesting effect, he notes, is that in Saturn's massive storm, at least, the observations can be matched by having particles of mixed composition, or
clouds of
water ice existing side - by - side with
clouds of ammonia
ice.
At first, the gas and dust
cloud is extremely cold and simple molecules such as carbon monoxide and
water settle on the grains of dust and solidify into
ice.
The presence of
water ice, he says, supports the idea that Saturn's superstorms are powered by condensation of
water and originate deep in the atmosphere, about 200 kilometers below the visible
cloud deck.
Why it matters: Arctic mixed - phase
clouds are complex because they consist of both
ice and
water.
The climate sensitivity classically defined is the response of global mean temperature to a forcing once all the «fast feedbacks» have occurred (atmospheric temperatures,
clouds,
water vapour, winds, snow, sea
ice etc.), but before any of the «slow» feedbacks have kicked in (
ice sheets, vegetation, carbon cycle etc.).
Of particular interest is a bright pit on the floor of crater Occator that exhibits probable sublimation of
water ice, producing haze
clouds inside the crater that appear and disappear with a diurnal rhythm.
«Probability density function,» a statistical representation of the likelihood of something occurring at any point in time, was used to examine
cloud properties, including vertical motion, liquid and
ice water content, and the conditions of
cloud particle growth, including how
ice crystals grow at the expense of liquid droplets.
Water droplets, ice crystals and water vapor are constantly changing and able to co-exist only when air in a cloud is constantly mo
Water droplets,
ice crystals and
water vapor are constantly changing and able to co-exist only when air in a cloud is constantly mo
water vapor are constantly changing and able to co-exist only when air in a
cloud is constantly moving.
The small amount of heat released when
water vapor condenses on
ice crystals in Arctic
clouds, which contain both
water and
ice, determines the
cloud's survival, according to scientists from Pacific Northwest National Laboratory and Environment Canada.
Mars Odyssey spotted vast tracts of
water ice, and Mars Reconnaissance Orbiter saw «dry
ice» snowflakes falling from
clouds near the pole.
Results: A team led by Pacific Northwest National Laboratory (PNNL) researchers has presented two processes, or explanations, for how extra
ice crystals form in mixed - phase
clouds —
clouds containing both
water and
ice — which are prevalent throughout the Arctic.
«This imaging was part of an experiment checking the opacity of the atmosphere at night in Curiosity's location on Mars, where
water -
ice clouds and hazes develop during this season,» Mark Lemmon of Texas A&M University and a member of the camera team, said in a statement.
Although droplets are thousands of times more numerous, previous studies have shown that adding even a small number of
ice crystals to these
clouds can lead to a fast dissipation of the
cloud water.
The main mode, which is involved in the formation of
ice crystals in mixed - phase
clouds (
clouds formed by
ice particles and
water droplets), is the immersion freezing mode.
In one sentence: Researchers at Pacific Northwest National Laboratory found that when miniscule particles of airborne dust, thought to be a perfect landing site for
water vapor, are modified by pollution, they change
cloud properties via
ice crystal number concentration and
ice water content.
The study, published in the Journal of Geophysical Research, shows how a few
ice crystals can overcome numerous
water droplets in a heated battle for vapor within cold
clouds.