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 the multiple path at a later time than the energy that came back directly from the hail to the radar. Both are however on the same radial angle from the radar as the antenna did not have the time to turn significantly. The multipath echoes are then analyzed on the radar display as echoes extending in a radial direction behind the actual location of the hail/heavy rain core. The loss of energy by due to multiple reflections means weaker return echoes. The hail spike region has thus comparatively quite weaker echoes than the echoes directly from the hail or heavy