A number of instruments were placed on the ground across the path of a larg
e tornado that passed west of the town of Allison, Texas, on June 8, 1995.
The center of the tornado came within 660 m of the closest instrument, whic
h recorded a pressure drop of 55 mbar and a subsequent pressure rise of 60
mbar. During the lowest recorded pressures (near r = 660 m), there were lar
ge and rapid pressure fluctuations; the largest fluctuation was a 10-mbar s
pike lasting 2 s. A second instrument on the opposite side of the tornado r
ecorded a pressure drop of 26 mbar. From the pressure variations with time
P(t) at the two instruments, the variation of pressure with distance p(r) f
rom the center of the tornado has been deduced for r > 660 m. As r decrease
s, the measured pressure function p(r) drops more abruptly than would be ex
pected from conservation of angular momentum of air spiraling inward near t
he ground level.