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====Low-pressure areas==== {{Main|Extratropical cyclone}} [[File:Feb242007 blizzard.gif|thumb|right|Extratropical cyclonic snowstorm, February 24, 2007β(Click for animation.)]] [[Extratropical cyclone|Mid-latitude cyclones]] are [[low-pressure area]]s which are capable of producing anything from cloudiness and mild [[Winter storm#Snow|snow storms]] to heavy [[blizzard]]s.<ref name="ExtraLessonMillUni">{{cite web| title = ESCI 241 β Meteorology; Lesson 16 β Extratropical Cyclones | author = DeCaria| publisher = Department of Earth Sciences, [[Millersville University]]| date = December 7, 2005| url = http://www.atmos.millersville.edu/~adecaria/ESCI241/esci241_lesson16_cyclones.html | access-date = June 21, 2009 |archive-url = https://web.archive.org/web/20080208224320/http://www.atmos.millersville.edu/~adecaria/ESCI241/esci241_lesson16_cyclones.html |archive-date = February 8, 2008}}</ref> During a hemisphere's [[autumn|fall]], winter, and spring, the atmosphere over continents can be cold enough through the depth of the [[troposphere]] to cause snowfall. In the Northern Hemisphere, the northern side of the low-pressure area produces the most snow.<ref> {{cite journal |last = Tolme |first = Paul |title = Weather 101: How to track and bag the big storms |journal = Ski Magazine |volume = 69 |issue = 4 |page = 126 |date = December 2004 |url = https://books.google.com/books?id=t1DaXO7wF20C&pg=PA126 |issn = 0037-6159 }}</ref> For the southern [[mid-latitudes]], the side of a [[cyclone]] that produces the most snow is the southern side.
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