The role clouds play in the modification of global radiation is still.
a major uncertainty in the risk assessment of UV effects on ecologica
l systems and human health. This study presents cloud transmission dat
a obtained from measurements with Robertson-Berger meters and simultan
eous cloud observations. The global transmission of erythemally weight
ed irradiance depends strongly on cloud amount and can be described by
a cubic function. The comparison with results derived from long-term
records of total global irradiance indicates no statistically signific
ant difference between the attenuation of erythemal and total global r
adiation. The large variance of data results from lumping together dat
a from different cloud types. Classification of data according to clou
d forms yields a more statisfactory fit. The coefficient of the cubic
term characterizes the ability of various cloud forms to attenuate UV
radiation. It varies between 0.4 for high clouds and approximately 1.0
for cumulonimbus. This attenuation parameter allows a quantitative de
scription of the cloud influence on irradiance and therefore a more ac
curate risk assessment.