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Figure 1 – effect of angle of inclination on Insolation
♤ The sun’s rays with small angle traverse more of the atmosphere than rays striking at a large angle. Longer the path of sun’s rays, greater is the amount of reflection and absorption of heat by atmosphere. As a result the intensity of insolation at a place is less (figure 1). Angle of inclination of solar radiation depends on latitude of a place. The higher the latitude the less is the angle they make with the surface of the earth resulting in slant sun rays. Figure 1 show the winter Solstices in the Northern Hemisphere where angle of inclination is zero at 66 ½ N latitude.
Latitude | 0° | 20° | 40° | 60° | 90° |
December 22 (winter solstice) | 12h 00m | 10h 48m | 9h 8m | 5h 33m | ♤ m |
June 21(summer Solstice) | 12h | 13h 12m | 14h 52m | 18h 27m | 6 months |