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

By J. R. Simonson

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Additional resources for Computing Methods in Solar Heating Design

Example text

3 w :::J co ~- Cl) 0 co ~:::J Cl) I ~ a;- 0 (/) 5· a. 0 o. o. o. o. o. o. o. o. o. o. o. AZIM o. 25. 0 31. 27 27. 99 24. 85 24. 00 45. 77 44. 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

This figure illustrates angles w, b=G cos 6 cos w sin cf> c=G cos 6 cos w d=G cos6 e=G sin 6 f=G sin 6 sin cf> g=G sin 6 cos cf> h=G cos 6 sin w (al A, B, and C are normal and tangential to the Earth's surface.

Clount for each month and for the average year. Two tables of results are given for two declination relationships. 45° x sin(360 (284 + N)/365). As will be seen in the tables, the latter form of o produces considerable differences in the winter months of January and December on surf aces of increasing slope and is worst in the case of 90° vertical surfaces. For surfaces that face due south the optimum annual total occurs at a slope of 31° and at that slope the annual total is increased further to a maximum at a 25° W azimuth angle, so demonstrating the predominance of afternoon sun at Kew.

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