Consider the three major regions of the Sun's radiation: ultraviolet, visible and infrared. For each, describe the possible fates of the energy once it reaches the Earth's atmosphere, and be sure to highlight how their fates differ.
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The Answer is Ultraviolet radiation from the Sun can be absorbed by various gases in the Earth's atmosphere, such as ozone, and can also be scattered by particles in the atmosphere. This can lead to the warming of the stratosphere and the creation of the ozone layer. In contrast, visible radiation is able to penetrate the Earth's atmosphere and reach the surface, where it can be absorbed by land, water, and vegetation, leading to heating and the production of infrared radiation. Infrared radiation, on the other hand, is absorbed by greenhouse gases in the atmosphere, such as carbon dioxide and water vapor, leading to the warming of the Earth's surface. These different fates of the Sun's radiation in the Earth's atmosphere ultimately contribute to the complex and interconnected processes that regulate the Earth's climate.

Consider the Three Major Regions of the Sun's Radiation: Ultraviolet