DIFFUSE-RADIATION MODELS AND MONTHLY-AVERAGE, DAILY, DIFFUSE DATA FOR A WIDE LATITUDE RANGE

Several years of measured data on global and diffuse radiation and sunshine duration for 40 widely spread locations in the latitude range 36 degrees S to 60 degrees N are used to develop and test models for estimating monthly-mean, daily, diffuse radiation on horizontal surfaces. Applicability of the clearness-index (K) and sunshine fraction (S/So) models for diffuse estimation and the effect of combining several variables into a single multilinear equation are tested. Correlations connecting the diffuse to global fraction (Hd/H) with K and S/So predict Hd values more accurately than their separate use. Among clearness-index and sunshine-fraction models, S/So models are found to have better accuracy if correlations are developed for wide latitude ranges. By including a term for declinations in the correlation, the accuracy of the estimated data can be marginally improved. The addition of latitude to the equation does not help to improve the accuracy further.