They've found that
the ice on comets has deuterium concentrations very similar to the water in our oceans.
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.
They are thought to occur when the Sun's heat vaporises newly exposed
ice on the comet, blasting dust off its surface.
When comets venture into the more intense sunlight of the inner solar system,
the ices on the comet nucleus begin to melt and fall away.
Not exact matches
Combining high resolution images and infrared spectra collected during the probe's approach, a team of nearly two dozen scientists pinpointed three patches of water
ice on the surface of the
comet's «upper» half.
If sunlight must penetrate the dust covering a
comet's water
ice in order to warm it and produce jets, Sunshine says the Deep Impact findings suggest the
ices on such dormant
comets may not have run out but merely become sealed — by layers of debris, for example.
Still, Chapman says, he would not be surprised to see water
ice on asteroids, adding that the distinction between
comets, traditionally considered to be icy, and asteroids, which have been largely thought of as rocky, is becoming increasingly blurred.
The
comet also contains more frozen carbon dioxide, or dry
ice, than has been found
on any other
comet.
Most
comets are bright with brilliant tails of evaporating
ice, and started life in the Oort cloud
on the solar system's edges.
The Rosetta spacecraft has detected biological components glycine and phosphorus emerging from its
comet - suggesting life
on Earth could have arrived
on a ball of
ice
DARMSTADT, GERMANY — The Rosetta orbiter
on Wednesday dropped a spidery, three - legged robot the size of a small refrigerator and watched as it tentatively set down
on a
comet — the first time that the surface of these primordial balls of dust and
ice has ever been explored.
The European Space Agency's Rosetta spacecraft has spotted an amino acid
on the
comet it orbits — confirming that a ball of
ice and dust can hold a major building block of life.
Based
on studies of
comets, researchers believe that these young solar systems swirl with
ice crystals and wispy gases that coalesce into gas giants like Saturn and Jupiter.
The European Space Agency's Rosetta spacecraft has spotted an amino acid
on the
comet it orbits — confirming that a ball of
ice and dust can hold one of life's major building blocks.
So it is possible that a crack has opened up
on the
comet's nucleus, which is less than about 3 kilometres across, exposing fresh
ice to the Sun.
Such organic - rich
ice may have arrived
on Mercury through
comet or asteroid impacts.
For five
ices, including carbon monoxide and methane, the researchers compared levels
on the sun - drenched side of the
comet to the shaded side.
In addition to water, organic molecules, which could have been deposited
on the surface by crashing
comets, somehow would have to get through the thick shells of
ice for life to form, a situation that puts Saturn's geyser - spewing moon Enceladus at the top of Nimmo's list of potential spots for life.
It is theorized that the process may be similar to what happens
on comets, when water vapor lifts tiny particles of dust and
ice off the surface.
ESA's Rosetta spacecraft has provided evidence for a daily water -
ice cycle
on and near the surface of
comets.
Scientists have identified a ring of
ice, dust and young
comets around a star similar to our sun, shedding light
on how our own solar system may have developed.
The
comet appears to have undergone visible changes, including the changes in the size and number of surface features such as smooth patches, pits, and craters, and the loss of
ice vaporized by the Sun or blasted off its surface by the Solar Wind into its tail as well as failing back
on the object like snow, so that it appears to shrink,
on average, by 25 to 50 centimeters (9.2 to 19.7 inches) with each orbit around the Sun.
Meanwhile, a different physical process in the
comet's smooth mid-section was causing water
ice to vaporize and flow through porous material to escape as a cloud of water vapor at the same time (NASA news release, and page
on «fluffy snowballs;» David Shiga, New Scientist, November 18, 2010; and Astronomy Picture of the Day).
Ice on Mars, the Moon, and certainly
on hot Mercury, should disappear faster than
comets deposit it today.
which calculates effects of small impacts quite nicely, but after some experimentatiion, does not seem quite so good for
comet impacts
on ice.
And indeed it would be virtually impossible to show it was other than mere chance that
comet impacts occurred at the right time, especially given that it would still be necessary to show that the
ice sheet would care about
comets, which we also consider unlikely (see the good discussion — particularly Mauri Pelto's comments —
on this over at the Open Mind Blog).