
Debris fallout refers to debris lofted into the air by a tornado that falls back to the ground, and that can persist well after a tornado has lifted. Debris lofted by stronger tornadoes has been known to travel significant distances, upwards of 200 mi (320 km) on rare occasions. Debris fallout events can be detected on radar using dual polarization products, notably correlation coefficient. Most debris in excess of 1 lb (0.45 kg) is not moved a great distance; however, lighter objects—especially paper goods—can be absorbed by the storm's updraft and moved into its forward-flank downdraft where they can be transported further by non-tornadic downdraft winds.
The basic mechanism of debris fallout is debris lofted by a tornado's updraft winds high into the atmosphere. Charles E. Anderson completed the first study focusing on debris fallout on the F5 1984 Barneveld tornado, which produced a large survey revealing a trail of paper debris as wide as 23 mi (37 km) at 110 mi (180 km) from Barneveld and a roughly 85 mi (137 km) long path of heavy debris (>1 lb (0.45 kg)). A later study focusing on debris fallout discovered that debris from an intense tornado was lofted potentially as high as 12 km (7.5 mi) into the atmosphere over the 15–20 minutes after the tornado striking a location, before debris was moved further into the tornado's forward-flank downdraft. A photograph had been traced and discovered to have an average speed of 18 m/s (40 mph; 65 km/h) over 30 minutes. A 1993 analysis by Thomas P. Grazulis of 12,651 tornadoes found only 86 had reports of debris being transported over 5 mi (8.0 km) from its origin.
The height of a tornado debris signature is positively and non-linearly correlated with the speed of updraft winds, which is likely compounded by fallout. Debris that falls directly over the vortex can result in an increase in the size of the tornado debris signature on radar.