It has been suggested that the length of the solar cycle (SCL) is related t
o solar forcing of global climate change [Fris-Christensen and Lassen, 1991
]. Although no physical mechanism had been proposed, the relation seemed to
be supported by interesting correlations with several paleoclimate records
and, separately, with the 20th century Northern Hemisphere instrumental re
cord. Actually, what has been correlated is the quasi-sinusoidal Gleissberg
cycle which is slightly greater in the 18th century than in the 20th centu
ry. Using the pre-industrial record as a boundary condition, the SCL-temper
ature correlation corresponds to an estimated 25% of global warming to 1980
and 15% to 1997.