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Assessing the signals of the Hale solar cycle in temperature proxy records from Northern Fennoscandia
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2020 (Engelska)Ingår i: Advances in Space Research, ISSN 0273-1177, E-ISSN 1879-1948, Vol. 66, nr 9, s. 2113-2121Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

Eight proxy records of Northern Fennoscandian summer temperature variability were analyzed for the CE 1700–2000 period. Stable and statistically significant correlation between the summer temperature reconstructions and a quasi 22-year Hale solar cycle was found to be present through the entire study period. The revealed solar–climatic link is a result of the effect of a weak solar cycle signal on a climatic system having internal bi-decadal variability. Precise physical mechanisms to explain this link are far from clear but galactic cosmic ray flux appears a probable physical agent to mediate the solar effect to the lower troposphere. No evidence of a link between Northern Fennoscandian temperature and quasi 20-year planetary-tidal cycle was found.

Ort, förlag, år, upplaga, sidor
2020. Vol. 66, nr 9, s. 2113-2121
Nyckelord [en]
Solar activity, Solar–climatic connections, Dendroclimatology
Nationell ämneskategori
Geovetenskap och miljövetenskap Astronomi, astrofysik och kosmologi
Identifikatorer
URN: urn:nbn:se:polar:diva-8831DOI: 10.1016/j.asr.2020.07.038OAI: oai:DiVA.org:polar-8831DiVA, id: diva2:1625716
Tillgänglig från: 2022-01-09 Skapad: 2022-01-09 Senast uppdaterad: 2022-01-09Bibliografiskt granskad

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Förlagets fulltexthttps://www.sciencedirect.com/science/article/pii/S0273117720305470
I samma tidskrift
Advances in Space Research
Geovetenskap och miljövetenskapAstronomi, astrofysik och kosmologi

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