About 1.1 million cloud-to-ground lightning flashes were recorded by a ligh
tning positioning and tracking system in southeastern Brazil in 1993. The 1
-year continuous lightning data set is the first obtained in Brazil. It has
been analyzed for geographical distribution of total flash density, percen
tage of positive flashes, negative and positive flash densities, and negati
ve and positive flash peak currents. The dependence of the flash density an
d peak current on latitude, altitude. and soil resistivity was investigated
. Negative flash peak current was found to be inversely correlated with lat
itude, but no other significant correlation was found for flash density and
peak current with these parameters. Positive flashes were found to be cont
aminated by intracloud flashes. The maximum total, negative, and positive f
lash densities were 15.5, 9.1, and 7.7 flashes/km(2) per year, respectively
. The average percentage of positive flashes was 36.5%. The geometric means
of negative and positive peak current were 30.9 kA and 17.8 kA. The high d
ensity, high percentage and low average peak current of positive flashes fo
und in this study are probably a result of such a contamination. Neglecting
positive flashes below 15 kA, assuming that they correspond to intracloud
flashes erroneously identified by the system, the maximum positive and tota
l flash densities would be 3.9 flashes/km(2) per year and 11.7 flashes/km(2
) per year. The percentage and geometric mean peak current of positive flas
h would be 23% and 38.7 kA, respectively. The results are discussed in the
context of other similar measurements made at different parts of the world.