Point rainfall as measured by a rain-gauge is examined in terms of a s
pace and time dependent rain event. The rain event is determined such
that the total number of rain events in any one year account for at le
ast 80 per cent of the annual area rainfall. The remaining fraction of
annual rainfall is considered to be rainfall due to isolated unorgani
zed rain systems. A 1-year record from 19 digital rain-gauge recorders
over a 600 km(2) area in the vicinity of the Kennedy Space Flight Cen
ter is used. Each tipping bucket rain-gauge has a resolution of 1 minu
te 0.25 mm. Rain rates, duration, areas and frequency of occurrence ar
e presented for nearly 200 rain events identified in a single year. St
rong seasonal signals are seen particularly in extreme rain events, wh
ich produce more than 90 mm of rain per event, account for 60 per cent
of the total network rainfall but occur less than 22 per cent of the
time. A simulation of the detection of the extreme rainfall events by
a remote sensing system such as TRMM suggests that the satellite will
see only 10 per cent of the rainfall due to extreme rain events. The r
esults illustrate the difficulties of sampling convective rainfall, es
pecially over a continental tropical area such as Florida, by an orbit
ing platform.