Chapter 4, "Energy and Radiation" is one of the most important chapters of this book. In it we discovered that the energy received from the Sun drives many of the environmental processes acting at the surface of the Earth. As we look ahead to chapter 5, "Air Temperature" and beyond we'll see how important this material is. The absorption of longwave radiation and and the transfer of sensible heat affect the temperature of the air. When water changes phases it gains or loses latent heat, affecting the temperature of the surrounding environment.
Figure GR4.1 High sun angles and lack of clouds results in much insolation in the Sahara Desert (Landsat image). Courtesy NASA (Source)
Figure GR4.2 Low sun angles and high albedo results in very little absorbed solar radiation in the ice-covered continent of Antarctica. Courtesy Jim Yungel/NASA (Source)
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For Citation: Ritter, Michael E.
The Physical Environment: an Introduction to Physical Geography.
2006. Date visited. http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/title_page.html