Computing Methods in Solar Heating Design by J. R. Simonson

By J. R. Simonson

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Further scattering occurs owing to the presence of larger particles such as water droplets, natural and manmade aerosols (for example, volcanic dust and smoke) and at increased path length this leads to the red skies of sunrise and sunset. On clear days 15-20 per cent of the total irradiance on a horizontal earth surface is diffuse when the sun is relatively high. On cloudy days the amount of beam radiation depends on cloudiness and the solar altitude. The proportion of diffuse radiation is greatest on lightly clouded days.

18 13. 89 64. 42 74. 34 52. 18 52. 37. 58 73. 15 92. 59 SEP 51. 44 70. 71 71. 80 73. 91 70. 49 62. 15 68. 70 66. 37 51. 7 3 32. 29 41. 96 NOV 1 5. 05 2 3. 95 9. 52 1 0 5 3. 81 515. 4 w ::J 5· ~· a. Q) :::0

7. 3]. It uses t~e measured values of Hd and H, and requires the calculation of Rb, the monthly average daily ratio of beam irradiation on the inclined surface to beam irradiation on the horizontal surface. The computer program discussed previously calculated Rb for each hour of each day and, bI the addition of an averaging procedure, a set of twelve values of Rb can readily be obtained. For each day of the month the sum of Rbibn for all daylight hours is obtained, and this is divided by the sum of Ibn for the sa~e period.

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