Lightning results from the electrical fields that are created
when ice particles in clouds rub together.
Storm clouds become electrified
when ice particles collide with each other and with unfrozen droplets in the cloud.
Not exact matches
When high - energy ultraviolet light from the central star strikes a clump of dust and
ice grains, it drives electrons off the
particles.
But if scientists are able to gain a deeper understanding of which dust
particles best form
ice and which don't, they may be able to maximize precipitation
when clouds do form and stave off future droughts like the one that has beset California recently (ClimateWire, Aug. 4).
Much of the dust deposit east of the Rockies arrived in the last
ice age, which ended some 11,000 years ago,
when particles that had been ground up and transported by glaciers were deposited by meltwater streams.
Intermittent phases of boiling, similar to what happened
when Vinalia Faculae formed, may have occurred during this process, littering the surface with
ice and salt
particles that formed the Cerealia bright spot.
When the glacier starts to retreat, the frontal moraines are no longer protected by the
ice, and a sort of «geological chronometer» is triggered, as the rocks begin to accumulate beryllium - 10 and helium - 3 produced by
particles resulting from cosmic rays.
When neutrinos pass through ultra-clear-blue
ice, the collision produces a
particle — called a muon — that radiates blue light.
They're buried deep down in the
ice, but they register the flashes of light that emitted
when neutrinos interact with an atom and produces a new
particle called a muon as the moon — muon travels through the
ice, that's what lights it up.
One wouldn't think of
ice particles burning up
when they hit the atmosphere, but that is what happens?
When a neutrino collides with an atomic nucleus, a new
particle called a muon is produced, which emits a faint blue glow in the transparent
ice that the DOMs can detect.
Urine that it vented also left a residue
when tiny
particles hit the craft's panels, so Lorenz suggests that future missions to Enceladus could look for signatures of life if similar residue is found in the minuscule dents left on a detector by
ice grains from the plumes.
Researchers have been fascinated with Enceladus since July 2005,
when Cassini revealed plumes of
ice particles and water vapour shooting out from the moon's south pole.
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.
The
particles generated in this region can even reach Antarctica
when they are transported by the wind (Gassó et al., 2010) and contribute to
ice particles formation.
Understanding how dust
particles are affected by each type of pollution will shed light for researchers to account for all types of pollution
when computing which
particles may form
ice crystals in cold clouds.
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.
Scientists are working to understand their underlying processes, such as which
particle surface properties encourage or discourage
ice formation, called nucleation, so they can accurately simulate how, where, and
when clouds are formed.
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.
When the jeep drag you around the river, those small
particles of
ice can hit the face pretty hard.
When the
particles settle out in these regions, the black carbon makes snow and
ice darker, which in turn warms the
ice.
Wendler found that more than 10,000
ice particles per second pass through a square inch
when the katabatic winds are very strong.»
Soot
particles absorb the sun's heat and melt the
ice when they settle on glaciers.
It's a problem for the climate because the black soot
particles are just the right color to absorb heat from the sun, either in the upper atmosphere or
when it settles back down to earth on Arctic snow and
ice (
when soot - free, the polar
ice caps reflect a tremendous amount of light and heat back into Space, helping keep the planet cool).
Typical temperature - supersaturation regions can be identified for the «onset» of
ice nucleation of these different
particle types, but the various
particle sizes and activated fractions reported in different studies have to be taken into account
when comparing results obtained with different methodologies.