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Yesterday’s winter-spring storm produced lots of severe weather on its eastern flank, but it also generated a band of heavy snow to its west. Just to the east of Chicago, IL, the infamous “rain-snow” line helped to create a rather large snowfall gradient…Yet, much larger gradients came into play for the Jan. 26-28, 2015 snowstorm in the mid-Atlantic and Northeast U.S…To read the full story, click here - http://bit.ly/1mZpCwg
When the upper level winds (I’m talking altitudes of four to eight miles above the Earth’s surface) take on a high-amplitude wave pattern (Fig. 1), strong low-pressure systems often develop. Given the counter-clockwise wind flow around such lows in the Northern Hemisphere, surface or near-ground temperatures typically take on a similar wave-like pattern…To read the full story, click here - http://bit.ly/1LeUrs4
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