Definitions

The albedo is the ratio of the radiation of radiation reflect by an object to the energy incident upon it.

The atmospheric emissivity is the ratio of the radiant energy emitted per unit time per unit area by the atmosphere to the energy emitted by an ideal blackbody at the same temperature.

The emission temperature of a planet is the blackbody temperature required to achieve energy balance.

Energy balance requires that the absorbed solar energy equals the infrared radiation emitted to space.

The greenhouse effect is the warming of the planet that results from the radiative properties of the atmosphere.

Solar Constant is the average rate of solar energy received on a surface perpendicular to the incident radiation at an average distance from the sun. The solar constant of Earth is approximately 1367 Wm-2.

Thermodynamics is the study of the relationships between work, heat, and the different forms of energy.



The Verner E. Suomi Virtual Museum development funded in part by the National Science Foundation Grant #EAR9809458.  Material presented is Copyrighted (C) 1999 by Steve Ackerman and Tom Whittaker.  If you have questions or comments, please let us know!