The earth’s climate change in the 13th–15th millennia bc. Possible cause

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Data on the content of the cosmogenic isotope 14C in the Earth’s atmosphere make it possible to study variations in solar activity in past epochs. However, changes in the Earth’s climate over time also lead to a distortion of information about solar activity. This paper examines the time interval from the end of the 17th to the beginning of the 10th millennium BC. During this time, as is known, there were several periods of climate change on Earth. There were several warming events (Mayendorf, Allered) and cooling events (the Oldest, Ancient, and Late Dryas). The reasons for these changes have not yet been determined. It is shown that a possible cause of the cooling during the Ancient Dryas could be a decrease in solar activity.

作者简介

I. Kudryavtsev

Ioffe Institute, Russian Academy of Sciences; Central Astronomical Observatory of the Russian Academy of Sciences at Pulkovo

Email: igor.koudriavtsev@mail.ioffe.ru
St. Petersburg, Russia; St. Petersburg, Russia

V. Dergachev

Ioffe Institute, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: v.dergachev@mail.ioffe.ru
St. Petersburg, Russia

Yu. Nagovitsyn

Central Astronomical Observatory of the Russian Academy of Sciences at Pulkovo; State University of Aerospace Instrumentation

Email: nag-yury@yandex.ru
St. Petersburg, Russia; St. Petersburg, Russia

参考

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In the print version, the article was published under the DOI: 10.31857/S0016794025040112


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