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Chad Merry

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I am curious about something. I live in St.Louis and we getting another ice storm this weekend. My question is this, What causes snow? Why is it always freezing rain or sleet? If it is freezing out should it not snow??

 
You get freezing rain when warm wet air overrides a shallow layer of cold air that may only be a couple of thousand feet thick. Since it is raining above the layer of cold air, the raindrops freeze on the way down. The ground and objects at ground level are usually cold enough for any liquid rain to freeze upon contact.



 
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Chad,



Saw the explanation on the weather channel the other night. Basically, there is a warm layer of air between the clouds causing the snow and the cold ground layer.



So if it is cold enough to snow, the snow melts in the warmer upper layer and then refreezes making sleet or ice.



Chris
 
There is a very fine line sometimes between Snow, Sleet (a.k.a. Ice Pellets) freezing rain, and plain old rain.



First of all... all start out as a solid. If the solid precipitation falls to the ground through an entire layer of sub-freezing temperatures (or a very shallow layer of warm air only at the surface)... then it falls as snow.



If that solid precipitation falls through a deep enough warm layer at the surface... it will have melted enough to fall as plain old rain.



For freezing rain... The layer near the surface is below freezing and there is a shallow warm layer above it... The snow melts completely as it falls through the warm layer. The warm layer has to be shallow enough for the now liquid precipitation to be "supercooled" (in liquid state but just slightly below freezing). When it falls back through the very shallow freezing layer at the surface, it immediately freezes to any surface that is below freezing.



For Sleet (a.k.a. Ice Pellets), the process is nearly identical to freezing rain. The difference is the freezing layer close to the ground is deeper and the warm air above it is shallower. This causes the snow that falls through it to only partially melt. The precipitation then falls through the thicker layer of sub-freezing air near the surface, and re-freezes into a ball of ice before hitting the ground.
 

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