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The heat on the body, on objects, etc., that is directly produced by the radiation should be distinguished from the increase in air temperature.
The amount of radiation intercepted by a planetary body varies as the square of the distance between the star and the planet. The Earth's orbit and obliquity change with time, sometimes achieving a nearly perfect circle, and at other times stretching out to an eccentricity of 5%. The total insolation remains almost constant but the seasonal and latitudinal distribution and intensity of solar radiation received at the Earth's surface also varies (for example see a graph)...
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Common topics in this essay:
- Nuclear Radiation
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- Solar
- Radiation Therapy
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- RADIATION DETECTION IN VEGETABLE LEAVES:
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- The Effects of Solar Radiation
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