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    Solar Activity and Regional Climate

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    Author
    Ogurtsov, M. G.
    Kocharov, Grant E.
    Lindholm, M.
    Eronen, M.
    Nagovitsyn, Yu A.
    Issue Date
    2001-01-01
    Keywords
    periodicity
    anomalies
    Fennoscandia
    solar cycles
    temperature
    cycles
    solar activity
    climate change
    mathematical models
    statistical analysis
    reconstruction
    Holocene
    paleoclimatology
    Europe
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    absolute age
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    Citation
    Ogurtsov, M. G., Kocharov, G. E., Lindholm, M., Eronen, M., & Nagovitsyn, Y. A. (2001). Solar activity and regional climate. Radiocarbon, 43(2A), 439-447.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.
    URI
    http://hdl.handle.net/10150/654638
    DOI
    10.1017/S0033822200038303
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We performed a statistical analysis of the data on summer temperature anomalies in northern Fennoscandia (8-1995 AD) and found that a 70-130-yr cycle is present in this series during most of the time period. A comparison of the reconstructed northern Fennoscandia temperature with different indicators of solar activity (Wolf numbers, the length of solar Schwabe cycle, extended bi-decadal radiocarbon series, and data on sunspots observed by naked eye) shows that the more probable cause of the periodicity is the modulation of regional northern Fennoscandia climate by the long-term solar cycle of Gleissberg. The effect of this century-scale solar modulation of the global Northern Hemisphere temperature is weaker.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200038303
    Scopus Count
    Collections
    Radiocarbon, Volume 43, Number 2A (2001

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