Journal cover Journal topic
Annales Geophysicae An open-access journal of the European Geosciences Union
Ann. Geophys., 20, 115-120, 2002
http://www.ann-geophys.net/20/115/2002/
doi:10.5194/angeo-20-115-2002
© Author(s) 2002. This work is distributed
under the Creative Commons Attribution 3.0 License.
 
31 Jan 2002
The ~ 2400-year cycle in atmospheric radiocarbon concentration: bispectrum of 14C data over the last 8000 years
S. S. Vasiliev and V. A. Dergachev Ioffe Physico-Technical Institute, Politekhnicheskaya, 26, St. Petersburg, 194021, Russia
Correspondence to: V. A. Dergachev
(v.dergachev@pop.ioffe.rssi.ru)
Abstract. We have carried out power spectrum, time-spectrum and bispectrum analyses of the long-term series of the radiocarbon concentrations deduced from measurements of the radiocarbon content in tree rings for the last 8000 years. Classical harmonic analysis of this time series shows a number of periods: 2400, 940, 710, 570, 500, 420, 360, 230, 210 and 190 years. A principle feature of the time series is the long period of ~ 2400 years, which is well known. The lines with periods of 710, 420 and 210 years are found to be the primary secular components of power spectrum. The complicated structure of the observed power spectrum is the result of ~ 2400-year modulation of primary secular components. The modulation induces the appearance of two side lines for every primary one, namely lines with periods of 940 and 570 years, of 500 and 360 years, and 230 and 190 years. The bispectral analysis shows that the parameters of carbon exchange system varied with the ~ 2400-year period during the last 8000 years. Variations of these parameters appear to be a climate effect on the rate of transfer of 14C between the atmosphere and the the ocean.

Key words. Meteorology and atmospheric dynamics (climatology; ocean-atmosphere interaction; paleoclimatology)


Citation: Vasiliev, S. S. and Dergachev, V. A.: The ~ 2400-year cycle in atmospheric radiocarbon concentration: bispectrum of 14C data over the last 8000 years, Ann. Geophys., 20, 115-120, doi:10.5194/angeo-20-115-2002, 2002.
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