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A photograph of a snowflake by W.A. Bentley shows off the lacy, intricate
pattern formed by the crystal.
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With Old Man Winter on the way, it seems
fitting to explore some questions about snow.
How does a snowflake form?
There are two ways that snow crystals form
in clouds. At warmer temperatures, snow condenses on small dust particles
that are suspended in the cloud, forming tiny droplets that freeze. This
process is called heterogeneous nucleation. When the air temperature
drops below negative-40 Celsius, water vapor converts directly to ice
through a process called homogenous nucleation.
What gives a snowflake its intricate
form?
The lacy, intricate pattern of a snowflake is determined
by the atmospheric conditions experienced by the crystal as it forms.
As an ice crystal descends through the atmosphere, it encounters variations
in temperature and humidity. Snow crystals tend to form simpler shapes
at a lower humidity and more complex shapes when the humidity is high.
Colder temperatures produce snowflakes with sharper tips and branched
arms or dendrites, while warmer conditions allow snowflakes to grow more
slowly, resulting in smoother, less intricate shapes - those sticky,
fluffy flakes that are ideal for snowball-making!
Is it true that no two snow crystals are alike?
This is probably one of the most frequently asked questions
about snow. The answer depends largely upon how you define the word "alike." The
short answer is that it's unlikely that any two snowflakes are absolutely
identical. Because each snow crystal experiences a different growth history
as it forms, it is improbable that any two snowflakes would be identical.
This article is just the tip of the proverbial iceberg
when it comes to information about snow. Visit the Jericho Historical
Society's Web site (http://snowflakebentley.com/jhs.htm) to learn more
about W.A. Bentley's legacy, or look for the photography collection Snow
Crystals by W.A. Bentley and W.J. Humphreys at your local library. It
will give you a new appreciation for the white stuff!
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