A MULTIPYRANOMETER METHOD FOR OBTAINING THE SOLAR BEAM AND DIFFUSE-RADIATION COMPONENTS - VALIDATION STUDIES

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Abstract

We discuss some of the practical issues associated with the use of a stationary multipyranometer system for determining both the beam and diffuse components of solar radiation, and the global insolation on arbitrary inclined planes. Results from a full year of validation measurements are presented and compared with (a) the values obtained using conventional, clock-driven, instrumentation (in the case of the direct beam component); and (b) with model-derived results (in the case of total insolation on inclined planes). The yearly average rms error for the beam component is found to be 50 W/m2 (using 10 min data) or 47 W/m2 (using hourly totals). The corresponding rms error for the horizontal global radiation is 18 W/m2 (for 10 min data). In the case of total insolation on arbitrary inclined planes, the rms errors are found to be smaller than 30 W/m2, which is comparable to the accuracy given by the best anisotropic-diffuse models currently available.
Original languageEnglish
Title of host publicationCLEAN AND SAFE ENERGY FOREVER, VOLS 1-3
Pages2112-2116
StatePublished - 1990

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