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January thaw driven by Chinook windsA key factor driving this warm-up is the Chinook wind, which is common this time of year. The Chinook wind is a warm, dry wind that originates in the Pacific Northwest, moving up into the ...
This type of wind in the Rockies is known as a chinook, and it often produces rapid temperature changes, particularly in winter. Chinook winds are the result of air rising over mountain ranges.
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