Natural Factors of Radiative Forcing
q Since the late 1970s, satellite instruments have observed small
oscillations due to the 11-year solar cycle. Mechanisms for the
amplification of solar effects on climate have been proposed,
but currently lack a rigorous theoretical or observational basis.
q Stratospheric aerosols from explosive volcanic eruptions lead to
negative forcing, which lasts a few years. Several major
eruptions occurred in the periods 1880 to 1920 and 1960 to
1991.
q The combined change in radiative forcing of the two major
natural factors (solar variation and volcanic aerosols) is
estimated to be negative for the past two, and possibly the past
four, decades.