J. Matthijsen et al., Reduction of solar UV by clouds: A comparison between satellite-derived cloud effects and ground-based radiation measurements, J GEO RES-A, 105(D4), 2000, pp. 5069-5080
Assessment of the effects of ozone depletion on biologically effective sola
r UV at ground level has been greatly advanced through the use of remote se
nsing data. Satellite data on atmospheric properties allow the construction
of geographically distributed surface UV radiation maps based on radiative
transfer calculations. In this respect, clouds play a dominant but rather
complex role. We compared the reduction of daily UV doses due to clouds, as
derived from satellite cloud data, with the reduction derived from routine
ground-based measurements of global solar radiation (i.e., broadband total
solar irradiances with wavelengths between 0.3 and 2.8 mu m). An empirical
relationship is used to link the reduction due to clouds of global solar r
adiation and UV radiation. The abundance of global solar radiation measurem
ents (data from over 125 stations in 30 satellite grid cells) for the Europ
ean region ensured a sound basis for the data analysis for the period consi
dered (May, June, and July of 1990, 1991, and 1992). Approximately 6500 dai
ly UV-reduction factors, defined as the ratio of daily UV doses calculated
with and without clouds, were thus obtained applying both methods. The dail
y UV-reduction factors (and 10-day averaged UV reduction factors) from the
two independent sources correlated well, with r(2) = 0.83 (r(2) = 0.89), an
d had a standard deviation of 0.06 (0.03). Over 90% of the satellite-derive
d results agreed within a range of +/-0.14 (+/-0.07) with the ground-based
measurement-derived results. We evaluated sources of uncertainty related to
spatial and temporal resolution, and optical properties, and estimated the
ir consequences and range. Among these different sources the largest uncert
ainties are caused by the sampling error, i.e., grid-cell average versus st
ation average, which is on average 0.10 for daily UV-reduction factors. Inf
ormation on the atmospheric optical properties during the measurements may
reduce the stated range of uncertainty from +/-0.14 to +/-0.07. The variati
on of the measurements from station to station is then the limiting factor.
We concluded that the reduction of daily UV based on satellite-derived clo
ud cover and cloud optical thickness relates well with the UV reduction due
to clouds derived from ground-based global solar radiation measurements.