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VIII/VI: Persistence of the Gleissberg (88-yr) Solar Cycle over the Last 10,000 Years: Evidence from Cosmogenic Isotopes

Title: Persistence of the Gleissberg (88-yr) Solar Cycle over the Last 10,000 Years: Evidence from Cosmogenic Isotopes  
Author: Paul E. Damon  
Affil: University of Arizona
Email: damon@geo.arizona.edu

Authors: Alexei N. Peristykh
Affils: University of Arizona

Abstract: Although there are other significant periods in the Fourier spectrum of tex2html_wrap_inline1212C time series (Damon and Sonett, 1991), the Gleissberg cycle is unique because it can be directly related to solar activity. The cycle was detected by Gleissberg through a low-pass filtering, secular smoothing (Gleissberg, 1944), of both height and length of sunspot cycle (Gleissberg, 1958). Frequency modulation (FM) as well as amplitude modulation (AM) of Schwabe cycle has been known for a long time (Vitinsky, Kopecky and Kuklin, 1986; Peristykh, 1993). We have previously pointed out that the change in solar cycle length means that some regular process originating inside the Sun with the period of 88 yrs frequency modulates the Schwabe cycle (Damon and Peristykh, 1999).

Stability of the Gleissberg cycle is of great interest. For that reason we have examined the longest cosmogenic isotope record provided by tex2html_wrap_inline1214C - INTCAL98 calibration record. The full record extends back to tex2html_wrap_inline41911,600 yrs (before AD 1950). During this period of time despite small gaps (requiring interpolation) the Gleissberg cycle has a period of 87.8 yrs. If we restrict our analysis to the last tex2html_wrap_inline4199,140 yrs (before AD 1950) where there are no gaps and no significant effect of interpolation we still obtain the period of the Gleissberg cycle equal to 87.8 yrs (Damon and Peristykh, 2000). However, time-frequency analysis (e.g., by the spectrogram method) indicates small variations in period during the whole time interval thus showing that there is some nonstationarity in the process expressed by the data.

The possibility that the Gleissberg cycle is related to forcing of past climate change during the entire Holocene is of great interest.

Damon, P.E. and C.P.Sonett (1991). Solar and terrestrial components of the atmospheric tex2html_wrap_inline1214C variation spectrum. In: The Sun in Time, p.360.

Damon, P.E. and A.N.Peristykh (1999). Solar cycle length and 20th century Northern Hemisphere warming: Revisited. Geophys.Res.Lett., 26, 2469.

Damon, P.E. and A.N.Peristykh (2000). Radiocarbon calibration and application to geophysics, solar physics, and astrophysics. Radiocarbon, 42, 137.

Gleissberg, W. (1944). A table of secular variations of the solar cycle. Terr.Magn.Atm.Electr., 49, 243.

Gleissberg, W. (1958). The eighty-year sunspot cycle. J.Brit.Astr.Assoc., 68, 148.

Peristykh, A.N. (1993). On frequency modulation of Schwabe cycle of solar activity by longer cycles. Eos,Trans.,AGU, 74(43, Suppl.), 491.

Vitinsky, Yu.I., M.Kopecky and G.V.Kuklin (1986). Statistics of the Sunspot Formation Activity of the Sun. Moscow, Nauka Publ., 1986.


next up previous contents index
Next: VIII: Possible Solar Modulation Up: Session VIII Previous: VIII: Galactic cosmic rays

Peter Fox
Tue Jun 12 11:56:17 MDT 2001