Snow… so pretty, so cold, so simple. Or is it?
At first glance, snow might seem pretty simple.
When cold air and water mix, you get snow, right?
Not quite.
The air must get cold enough to freeze as vapour in the clouds before it starts falling to the ground.
If it freezes after it has started falling, you might get ice, sleet, graupel, freezing fog, hail, or any other number of other frozen precipitation types instead of snow.
So how cold does the air need to be to make snow?
Well… the best temperature for snow is between about 0 °C (32 °F) and −40 °C (−40 °F).
Snowflakes often start forming when vapour sticks to dust in a cloud.
The vapour freezes, forming crystal faces — six of them to be exact.
When more vapour begins to freeze on the surface of the ice crystals, they get heavy enough to fall from the clouds.
Voila! A snowflake is created!
But snow isn’t just fun…
It’s also a critical part of regulating global temperatures. While the snow lays there waiting to be turned into a friendly snowman, it’s also cooling the ground and air around it.
An estimated 68% of the world’s supply of freshwater stays trapped in ice and snow. This makes snowfall a critical part of life on Earth!
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