La presión de radiación es la presión ejercida sobre cualquier superficie expuesta a la radiación electromagnética. Si la radiación es absorbida, la presión es la densidad del flujo de la energía dividida por la velocidad de la luz. Si la radiación es totalmente reflejada, la presión de radiación se duplica. Por ejemplo, la radiación del Sol en la Tierra tiene una densidad de flujo de 1370 W/m2; por lo, tanto la presión de radiación es 4,6 μPa (absorbida) (véase modelo climático).

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Radiation pressure is the pressure exerted upon any surface exposed to electromagnetic radiation. Radiation pressure implies an interaction between electromagnetic radiation and bodies of various types, including clouds of particles or gases. The interactions can be absorption, reflection, or some of both (the common case). Bodies also emit radiation and thereby experience a resulting pressure. The forces generated by radiation pressure are generally too small to be detected under everyday circumstances; however, they do play a crucial role in some settings, such as astronomy and astrodynamics. For example, had the effects of the sun's radiation pressure on the spacecraft of the Viking program been ignored, the spacecraft would have missed Mars orbit by about 15,000 kilometers. This article addresses the macroscopic aspects of radiation pressure. Detailed quantum mechanical aspects of interactions are addressed in specialized articles on the subject. The details of how photons of various wavelengths interact with atoms can be explored through links in the See also section.

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