Climate Sensitivity - Radiative Forcing Functions

Radiative Forcing Functions

A number of different inputs can give rise to radiative forcing. In addition to the downwelling radiation due to the greenhouse effect, the IPCC First Scientific Assessment Report listed solar radiation variability due to orbital changes, variability due to changes in solar irradiance, direct aerosol effects (e.g., changes in albedo due to cloud cover), indirect aerosol effects, and surface characteristics.

Read more about this topic:  Climate Sensitivity

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    Robert Frost (1874–1963)

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    William Wordsworth (1770–1850)