Articles | Volume 22, issue 3
https://doi.org/10.5194/cp-22-461-2026
https://doi.org/10.5194/cp-22-461-2026
Research article
 | 
04 Mar 2026
Research article |  | 04 Mar 2026

Seven centuries of rainfall reconstructed from Scots Pine ring width in sub-Arctic Sweden

Petter Stridbeck, Jesper Björklund, Fredrik Charpentier Ljungqvist, Jennie Sandström, Mauricio Fuentes, Paul J. Krusic, Zhi-Bo Li, and Kristina Seftigen

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Cited articles

Arosio, T., Leuenberger, M., Nicolussi, K., Esper, J., Krusic, P., Bebchuk, T., Tegel, W., Hafner, A., Kirdyanov, A. V., Schlüchter, C., Reinig, F., Muschitiello, F., and Büntgen, U.: Tree-ring stable isotopes from the European Alps reveal long-term summer drying over the Holocene, Science Advances, 11, eadr4161, https://doi.org/10.1126/sciadv.adr4161, 2025. 
Bebchuk, T., Moir, A. K., Arosio, T., Kirdyanov, A. V., Torbenson, M. C. A., Krusic, P. J., Hindson, T. R., Howard, H., Buchwal, A., Norman, C. A. P., and Büntgen, U.: Taxus tree-ring chronologies from southern England reveal western European hydroclimate changes over the past three centuries, Clim Dyn., 63, 108, https://doi.org/10.1007/s00382-025-07601-2, 2025. 
Bingham, C., Godfrey, M., and Tukey J.: Modern techniques of power spectrum estimation, IEEE Transactions on Audio and Electroacoustics, 15, 56–66, https://doi.org/10.1109/TAU.1967.1161895, 1967. 
Björklund, J., Seftigen, K., Stoffel, M., Fonti, M. V., Kottlow, S., Frank, D. C., et al.: Fennoscandian tree-ring anatomy shows a warmer modern than medieval climate, Nature, 620, 97–103, https://doi.org/10.1038/s41586-023-06176-4, 2023. 
Briffa, K. R., Jones, P. D., Bartholin, T. S., Eckstein, D., Schweingruber, F. H., Karlén, W., Zetterberg, P., and Eronen, M.: Fennoscandian summers from AD 500: Temperature changes on short and long timescales, Clim Dyn., 7, 111–119, https://doi.org/10.1007/BF00211153, 1992. 
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Here we present the first tree-ring-based reconstruction of precipitation in sub-Arctic Sweden, extending back to medieval times. The reconstruction is derived from living and dead Scots pine growing in the rocky, drought-prone High Coast region (63° N). Unlike most high-latitude conifers that are typically limited by temperature, these trees thrive during cool, cloudy, and wet summers. This rare response enabled filling a significant gap in our understanding of historical climate variability.
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