The Angstrom turbidity coefficient, the Linke turbidity factor, and the Uns
worth-Monteith coefficient have been determined and analysed based on measu
rements of normal direct irradiance and global horizontal irradiance taken
in Valencia, Spain, between January 1990 and December 1996. The data, which
were acquired automatically and continuously, have been filtered to select
only those values corresponding to clear sky conditions. To determine the
Angstrom turbidity coefficient the method proposed by Louche et al. has bee
n used whilst the expression for delta(CDA) proposed by Kasten was used to
obtain the Linke turbidity coefficient. The Angstrom turbidity coefficient
showed a minimum in winter with values between 0.06 and 0.12. It tended to
increase in the spring and reach a maximum between 0.22 and 0.29 in summer
before falling again in the autumn. The daily and annual evolution of all t
hree coefficients were very similar with correlation coefficients between p
airs of them close to 1. (C) 1999 Elsevier Science Ltd. All rights reserved
.