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By J. R. Simonson

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Inclined surface radiation measurements at Cardiff', The National Radiation Centre, Helios No. 9, published by The Solar Energy Unit, University College, Cardiff, 1980, pp. 10-11. , An appraisal of solar water heating, Final Year project, Department of Mechanical Engineering, The City University, London, June 1978. , 'Calculating the position of the Sun', Solar Energy, Vol. 20, pp. 393-397 (1978). 3 The Calculation of Incident Radiation In the previous chapter it was seen that it is impracticable to attempt to measure solar irradiance on other than horizontal surfaces at selected locations, and in this chapter it will be shown how this measured irradiance is used in the calculation of incident irradiation on collector surfaces.

1 by putting the slope S = 0° for a horizontal surface. 1. 6) It is necessary therefore to calculate Rb at the mid-point of each hour for each of the daylight hours throughout the year. As Rb is calculated at the mid-point of each hour it is useful also to have available 8 at the mid-point of each hour for the purposes of calculating (ta)/(ta)n, as described in the next chapter. This is the ratio of the transmittance-absorptance product of the solar collector at the angle of incidence 8 to the value normal to the collector.

G. Lof et al. World Distribution of Solar Energy, Engineering Experiment Station Report 21, University of Wisconsin, Madison, Wisconsin, 1966. Climate types: Cf Aw Bs Cs Am BW mesothermal forest, moist, rainfall throughout the year tropical forest, dry in winter. Steppe or semi-arid mesothermal forest, dry in winter. tropical forest, monsoon rain, short dry season. desert or semi-arid. 17) The above correlations for diffuse irradiation are based on measured global irradiation and extraterrestrial irradiation, respectively.

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