Mid-February 2014 North American winter storm of further-north Georgia received unusually heavy snows. Precipitation started as light rain late on the 10th, with significant snow by the following morning while still above freezing, turning back to light rain before ending by mid-day. More light rain began after midnight, changing to snow as temperatures fell, then to sleet, freezing rain, back to sleet again before another significant snow by the morning of the 13th. Areas north of the city generally got mostly snow and sleet, while a large swath from the south metro area eastward got the heaviest ice accumulations, though a dry slot at mid-day proved
Hail spike rain core. Since hail cores are most intense at higher elevations, hail spikes usually appear at the levels aloft that accompany the most intense hail. Because of this, hail spikes are usually not seen at lower elevations. Another restriction to detection is that the signal of the radar beam has to do multiple reflections, each time weakening it, and are therefore usually noticeable only in extremely large hailstone cases. In rare cases more than one hail spike has been documented with a single storm in one volume scan. This indicates that more than one hail core exists in the same