Snow storm is most likely found along the comma tail of the mid-latitude cyclone
Large moving atmospheric cyclonic storms with a center of low air pressure, known as mid-latitude or frontal cyclones, can have a diameter of up to 2000 kilometers. An strong mid-latitude cyclone may have a surface pressure as low as 970 millibars, compared to an average sea-level pressure of 1013 millibars.
Individual mid-latitude cyclones typically last between three and ten days while migrating mostly from west to east. The primary meteorological phenomenon in the Earth's mid-latitudes is a frontal cyclone, which develops along the polar front. Mid-latitude cyclones form when warm tropical and cold polar air masses collide at the polar front.
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