Images taken by geostationary satellites may be used to estimate solar
irradiance fluxes at the earth's surface. The Heliosat method is a wi
dely applied procedure for this task. It is based on the empirical cor
relation between a satellite derived cloud index and the irradiance at
the ground. Modifications to this procedure that may reduce the tempo
ral variability of the correlation are presented. The modified method
may open the way to the use of a generic relation of cloud index and g
lobal irradiance.