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Growing seasons of Nordic mountain birch in northernmost Europe as indicated by long-term field studies and analyses of satellite images

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Abstract

The phenophases first greening (bud burst) and yellowing of Nordic mountain birch (Betula pubescens ssp.tortuosa, also called B. p. ssp. czerepanovii) were observed at three sites on the Kola Peninsula in northernmost Europe during the period 1964–2003, and at two sites in the trans-boundary Pasvik-Enare region during 1994–2003. The field observations were compared with satellite images based on the GIMMS-NDVI dataset covering 1982–2002 at the start and end of the growing season. A trend for a delay of first greening was observed at only one of the sites (Kandalaksha) over the 40 year period. This fits well with the delayed onset of the growing season for that site based on satellite images. No significant changes in time of greening at the other sites were found with either field observations or satellite analyses throughout the study period. These results differ from the earlier spring generally observed in other parts of Europe in recent decades. In the coldest regions of Europe, e.g. in northern high mountains and the northernmost continental areas, increased precipitation associated with the generally positive North Atlantic Oscillation in the last few decades has often fallen as snow. Increased snow may delay the time of onset of the growing season, although increased temperature generally causes earlier spring phenophases. Autumn yellowing of birch leaves tends towards an earlier date at all sites. Due to both later birch greening and earlier yellowing at the Kandalaksha site, the growing season there has also become significantly shorter during the years observed. The sites showing the most advanced yellowing in the field throughout the study period fit well with areas showing an earlier end of the growing season from satellite images covering 1982–2002. The earlier yellowing is highly correlated with a trend at the sites in autumn for earlier decreasing air temperature over the study period, indicating that this environmental factor is important also for autumn phenophases.

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Acknowledgements

This work was financed by the project ‘Phenology as an indicator of climate change effects’ (PhenoClim), sponsored by the Norwegian Research Council, contract 155904/720. Financial contributions to the study have also been given by the Norwegian Ministry of Environment and the County Governor of Finnmark. We are thankful to all persons in Russia and Norway who participated in data collection and to Martin Smith for his careful correction of the English language.

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Authors and Affiliations

  1. Department of Biology, University Oslo, Blindern, Oslo, Norway

    F. E. Wielgolaski

  2. Kandalaksha zapovednik, Kandalaksha, Russia

    E. Shutova

  3. NORUT IT, Tromsø, Norway

    S. R. Karlsen & K. A. Høgda

  4. Pasvik zapovednik, Rajakoski, Russia

    O. Makarova

  5. Bioforsk Soil and Environment Svanhovd, Svanvik, Norway

    E. Haraldsson, P. E. Aspholm & L. Flø

  6. Lapland Zapovednik, Monchegorsk, Russia

    N. Berlina

  7. Polar-Alpine Botanical Garden-Institute, Kirovsk, Russia

    T. Filimonova

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  1. E. Shutova
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  2. F. E. Wielgolaski
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  10. K. A. Høgda
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Correspondence to F. E. Wielgolaski.

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Shutova, E., Wielgolaski, F.E., Karlsen, S.R. et al. Growing seasons of Nordic mountain birch in northernmost Europe as indicated by long-term field studies and analyses of satellite images. Int J Biometeorol 51, 155–166 (2006). https://doi.org/10.1007/s00484-006-0042-y

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  • DOI: https://doi.org/10.1007/s00484-006-0042-y

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