In climate science, radiative forcing is generally defined as the change in net irradiance between different layers of the atmosphere. Typically, radiative forcing is quantified at the tropopause in units of watts per square meter. A positive forcing (more incoming energy) tends to warm the system, while a negative forcing (more outgoing energy) tends to cool it. Sources of radiative forcing include changes in insolation (incident solar radiation) and in concentrations of radiatively active gases and aerosols.
Read more about Radiative Forcing: Radiation Balance, IPCC Usage, Climate Sensitivity, Related Measures
Famous quotes containing the word forcing:
“An empty head is not really empty; it is stuffed with rubbish. Hence the difficulty of forcing anything into an empty head.”
—Eric Hoffer (1902–1983)