It has been shown that the quasi-five-year and long-term (with a duration o
f several years) variations in the global air temperature are related to co
smic effects, whose intensity is modulated by the Ii-year solar cycle. Thes
e cosmic factors are shown to affect atmospheric processes, as a result of
which the temperature response lags behind the variations in the parameters
of these factors by 1.8 yr, on average. Such an effect can be exerted on t
he atmospheric circulation by high-energy particles of solar flares and cos
mic rays. The effect of the anthropogenic factor on the near-Earth air temp
erature has apparently increased beginning with the 1980s, resulting in an
additional temperature rise by 0.015 K/yr, on the average, during the perio
d from 1983 to 1995.