Halistatt Cycle Subarctic Fennoscandian Temperature and Its Possible Link with Solar Activity


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Reconstruction of summer temperature at subarctic Fennoscandia (68°–70° N, 20°–30° E), based on tree-ring data, was compared with three solar activity reconstructions, obtained by means of 14C and 10Be. It was shown that temperature proxy reconstructs well both long-term and short-term temperature variability. Weak, but significant positive correlation between reconstructed temperature (Helama et al., 2010) averaged over 40 years, and solar proxies was found during BC 5495–AD 1895. It was shown that Hallstatt cyclicity (1800–2300 years) is the main common feature in temperature and solar proxies. Possible mechanisms of the solar–temperature link over subarctic Fennoscandia are discussed.

作者简介

M. Ogurtsov

Ioffe Physico-Technical Institute; Central Astronomical observatory at Pulkov

编辑信件的主要联系方式.
Email: maxim.ogurtsov@mail.ioffe.ru
俄罗斯联邦, St. Petersburg; St. Petersburg

S. Helama

Natural Resources Institute Finland

Email: maxim.ogurtsov@mail.ioffe.ru
芬兰, Rovaniemi

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