The Hallstatt solar cycle from radiocarbon data


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The data on the 14C concentration in the Earth’s atmosphere are studied on a time span of 50000 years. It is shown that the Hallstatt cycle (a temporal variation with a period of 1500–2000 years) has been present in this series for at least 30000 years. However, this cycle is not purely of solar origin; nonsolar (supposedly climatic) factors contribute into it in certain epochs.

Sobre autores

M. Ogurtsov

Ioffe Physical-Technical Institute; Main (Pulkovo) Astronomic Observatory of the Russian Academy of Sciences

Autor responsável pela correspondência
Email: maxim.ogurtsov@mail.ioffe.ru
Rússia, St. Petersburg; St. Petersburg

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