Possible influence of solar and astronomical factors on a climate of Northern Fennoscandia

Abstract Eleven proxy records of Northern Fennoscandia and North Atlantic climate variability were analyzed. Correlation of climatic records with (a) a quasi 11-year solar cycle of Schwabe, (b) a quasi 22-year solar cycle of Heil, (c) a quasi 20-year planetary-tidal cycle, related to wobbling of the...

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Bibliographic Details
Published in:Journal of Physics: Conference Series
Main Authors: Ogurtsov, M G, Veretenenko, S V, Helama, S, Jalkanen, R, Lindholm, M
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2020
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Online Access:http://dx.doi.org/10.1088/1742-6596/1697/1/012007
https://iopscience.iop.org/article/10.1088/1742-6596/1697/1/012007/pdf
https://iopscience.iop.org/article/10.1088/1742-6596/1697/1/012007
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Summary:Abstract Eleven proxy records of Northern Fennoscandia and North Atlantic climate variability were analyzed. Correlation of climatic records with (a) a quasi 11-year solar cycle of Schwabe, (b) a quasi 22-year solar cycle of Heil, (c) a quasi 20-year planetary-tidal cycle, related to wobbling of the Sun around the baricenter of the solar system, has been studied. A weak but stable and statistically significant correlation between the climatic proxies of Northern Fennoscandia and a double solar cycle was found to be present through the AD 1700–2000. No evidence of a connection between climatic records and both solar Schwabe cycle and quasi 20-year astronomic cycle were found. Possible physical mechanisms behind the revealed effect are discussed.