When cold temperatures and high humidity levels combine in the atmosphere,
snow crystals form.
Each snow crystal forms when water vapor in the clouds condenses into ice.
Not exact matches
As long as they don't
form ice
crystals, these clouds won't shed more than a few flakes of
snow over the Sierras» 13,000 - foot peaks.
That frozen vapor quickly
forms ice
crystals that drop out of the cloud as
snow.
Depth hoar
crystals are
formed at the base of a snowpack when water vapor sublimates onto existing
snow crystals.
A well -
formed dendritic
snow crystal (like that shown in the first illustration) has six main arms that are 60 degrees apart, branches at 60 degrees from each arm and, sometimes, smaller branches on those branches.
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.
When the
snow gets packed down by subsequent layers, the space between the
crystals is eventually sealed off, trapping a small sample of the atmosphere in newly
formed ice.
Consequently in her Human
Snow Crystal, appears a human
form juxtaposed upon a cut out of a snowflake.
When the
snow gets packed down by subsequent layers, the space between the
crystals is eventually sealed off, trapping a small sample of the atmosphere in newly
formed ice.
Once an ice
crystal has
formed, it absorbs and freezes additional water vapor from the surrounding air, growing into a
snow crystal or
snow pellet, which then falls to Earth.
The transition from
snow to firn to ice occurs as the weight of overlying material causes the
snow crystals to compress, deform and recrystalize in more compact
form.