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Slide into oblivion
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Flakes study flakes
Let's quit fretting about billions of snowflakes and look at them as individuals, starting with the basics: Snow forms when water vapor in the air drops below the freezing point, and the vapor loses an amount of energy called the "heat of crystallization." A similar process forms ice, except that the water is a solid, not a vapor. (Snow can also be compressed into ice, as happens in glaciers and avalanches.) Due to the laws of thermodynamics -- none of which we Why Filers even pretend to grasp -- water vapor crystallizes most easily on a particle of, say, dust. Once the process starts, it cascades: water vapor in the air easily crystallizes onto existing water crystals. Because of the geometry of bonds between water molecules, snow flakes are all based on hexagons. Still, depending on temperature and humidity, the bonding can result in any number of shapes. And since conditions can change as the flake gets bounced around in a cloud, one shape can change into another; witness the plate-dendritic flake shown above.
All unique?
He suspects that the popular belief that every snow crystal looks different arose "as a kind of appreciation for the complicated design -- and because they're so beautiful."
Wang's actual excuse for studying frozen, airborne water is to figure out how it will affect global climate. Clouds, especially the high-flying cirrus clouds, are essentially formations of airborne ice, and
In other words, clouds could either amplify or dampen global warming. Wang says there are too many variables to know the correct answer, particularly since, as his graduate student Emily Liu just learned, the exact effect depends to some extent on the shape of the ice crystals. Slide on over to our "all-downhill-from-here" bibliography. |
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