Extreme rainfall events can have severe impacts on society, so possible lon
g-term changes in the intensity of extreme events are of concern. Testing f
or long-term changes in the intensity of extreme events is complicated by d
ata inhomogeneities resulting from site and instrumentation changes. Using
rainfall data from stations in South Africa that have not involved site rel
ocations, but which have not been tested for inhomogeneities resulting from
changes in instrumentation, a method of testing for changes in the intensi
ty of extreme events is adopted. Significant increases in the intensity of
extreme rainfall events between 1931-1960 and 1961-1990 are identified over
about 70% of the country. The intensity of the 10-year high rainfall event
s has increased by over 10% over large areas of the country, except in part
s of the north-east, north-west and in the winter rainfall region of the so
uth-west. Percentage increases in the intensity of high rainfall events an
largest for the most extreme events. While some inhomogeneities remain in t
he data used, the observed changes in the intensity of extreme rainfall eve
nts over South Africa are thought to be at least partly real.