To provide an accurate solar resource assessment, radiometric stations
measuring global, diffuse, and direct irradiance must be widespread.
Nevertheless, the high capital costs of thermopile instruments, usuall
y used in pyranometry, represent an important obstacle. Therefore, sil
icon photovoltaic sensors have emerged as a more accessible alternativ
e than standard thermopile sensors. However, their temperature and spe
ctral responses must be taken into account in order to match silicon c
ells and thermopile responses. Global and diffuse irradiance have been
measured from early 1990 to the end of 1992 in Almeria, southeastern
Spain. by means of thermopile and photovoltaic sensor. Polar axis shad
owbands were employed to measure the diffuse irradiance. These 10-minu
te coincident data sets, covering a complete range of atmospheric cond
itions, have been used to develop a correction procedure for the silic
on detector measurements. Before the correction procedure was applied
severe discrepancies were found, especially for the diffuse irradiance
measurements performed under clear skies. Results of the correction m
ethod applied to an independent data set show a remarkable improvement
. After correction, the comparison of silicon cell measurements with t
hose obtained by means of thermopile pyranometers leads to a root mean
square deviation of about 4% and 5% over the mean Value of global and
diffuse horizontal irradiance, respectively.