The frequency spectrum of Northern Hemisphere atmospheric CO2 concentration
shows strong periodicities at 6.2, 1.0 and 0.5 years. The 6.2 year cyclici
ty has been attributed to non-linear interactions between the annual cycle
and the atmospheric pole tide. The yearly signal is linked to terrestrial p
hotosynthesis; phase analysis shows that annual CO2 minima occur at a lag o
f approximately 85 days from insolation maxima. Variations in the nominal y
early period occur during times of anomalous anthropogenic CO2 production.
Periodicity at 6 months represents a deviation of the yearly signal from an
annual sinusoid. If the yearly signal is largely sinusoidal, a plausible s
ource of the 6 month periodicity could be cyclic phytoplankton productivity
driven by natural insolation modes. Together, the three largest spectral p
eaks account for over 99% of the variation in detrended CO2 data. Copyright
(C) 1999 Royal Meteorological Society.