Solar Activity and Regional Climate
| dc.contributor.author | Ogurtsov, M. G. | |
| dc.contributor.author | Kocharov, Grant E. | |
| dc.contributor.author | Lindholm, M. | |
| dc.contributor.author | Eronen, M. | |
| dc.contributor.author | Nagovitsyn, Yu A. | |
| dc.date.accessioned | 2021-02-11T21:33:08Z | |
| dc.date.available | 2021-02-11T21:33:08Z | |
| dc.date.issued | 2001-01-01 | |
| dc.identifier.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. | |
| dc.identifier.issn | 0033-8222 | |
| dc.identifier.doi | 10.1017/S0033822200038303 | |
| dc.identifier.uri | http://hdl.handle.net/10150/654638 | |
| dc.description | From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000. | |
| dc.description.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. | |
| dc.language.iso | en | |
| dc.publisher | Department of Geosciences, The University of Arizona | |
| dc.relation.url | http://radiocarbon.webhost.uits.arizona.edu/ | |
| dc.rights | Copyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved. | |
| dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | |
| dc.subject | periodicity | |
| dc.subject | anomalies | |
| dc.subject | Fennoscandia | |
| dc.subject | solar cycles | |
| dc.subject | temperature | |
| dc.subject | cycles | |
| dc.subject | solar activity | |
| dc.subject | climate change | |
| dc.subject | mathematical models | |
| dc.subject | statistical analysis | |
| dc.subject | reconstruction | |
| dc.subject | Holocene | |
| dc.subject | paleoclimatology | |
| dc.subject | Europe | |
| dc.subject | Cenozoic | |
| dc.subject | Quaternary | |
| dc.subject | C 14 | |
| dc.subject | carbon | |
| dc.subject | dates | |
| dc.subject | isotopes | |
| dc.subject | radioactive isotopes | |
| dc.subject | absolute age | |
| dc.title | Solar Activity and Regional Climate | |
| dc.type | Proceedings | |
| dc.type | text | |
| dc.identifier.journal | Radiocarbon | |
| dc.description.collectioninformation | The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information. | |
| dc.eprint.version | Final published version | |
| dc.description.admin-note | Migrated from OJS platform February 2021 | |
| dc.source.volume | 43 | |
| dc.source.issue | 2A | |
| dc.source.beginpage | 439 | |
| dc.source.endpage | 447 | |
| refterms.dateFOA | 2021-02-11T21:33:08Z |
