How does the Sun warm Earth through thermal radiation?

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The Sun warms Earth through the process of thermal radiation, which involves the transfer of energy in the form of electromagnetic radiation. Unlike other heat transfer methods, thermal radiation does not require an intervening medium to travel through space, allowing solar energy to reach Earth at the speed of light.1

This energy, often referred to as "shortwave" radiation, consists of wavelengths ranging from ultraviolet to infrared. Upon reaching Earth, a portion of this radiation is reflected back into space by clouds, the atmosphere, and the surface, while the remainder is absorbed by the planet. This absorption process is the primary mechanism by which the Sun heats Earth’s surface.1234

Once absorbed, this energy is systematically returned to space as "longwave" infrared radiation. The atmosphere plays a critical role in this cycle by trapping some of this outgoing heat—a process known as the greenhouse effect—which maintains the planet's surface temperature at a level capable of supporting life.32