A storm-intercept team from the University of Oklahoma, using the Los
Alamos National Laboratory portable, continuous wave/frequency modulat
ed-continuous wave, 3-cm Doppler radar, collected close-range data at
and below cloud base in six supercell tornadoes in the southern plains
during the springs of 1990 and 1991. Data collection and analysis tec
hniques are described. Wind spectra from five weak-to-strong tornadoes
and from one violent tornado are presented and discussed in conjuncti
on with simultaneous boresighted video documentation, photogrammetric
analysis, and damage surveys. Maximum Doppler wind speeds of 55-105 m
s-1 were found in five of the tornadoes; wind speeds as high as 120-12
5 m s-1 were found in a large tornado during an outbreak on 26 April 1
991. These may be the highest wind speeds ever measured by Doppler rad
ar and the first radar measurements of F-5 intensity wind speeds. The
variation in the spectrum across the 26 April 1991 tornado is presente
d. Standard and mobile soundings, and surface data, used to determine
the ''thermodynamic speed limit'' indicate that it was usually exceede
d by 50%-100%. A comparison of actual Doppler spectra with simulated s
pectra suggests that the maximum in radar reflectivity in supercell to
rnadoes lies well outside the core.