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Connecting potential frost damage events identified from meteorological records to radial growth variation in Norway spruce and Scots pine

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An Erratum to this article was published on 21 September 2017

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Abstract

Key message

Conifer radial growth reductions may be related to unusual snow conditions or a mismatch between frost hardiness level and minimum temperature, but not typically to low winter temperature extremes.

Abstract

The aim of this study was to examine if temperature conditions potentially causing frost damage have an effect on radial growth in Norway spruce and Scots pine in Finland. We hypothesized that frost damage occurs and reduces radial growth after (1) extreme cold winter temperatures, (2) frost hardiness levels insufficient to minimum temperatures, and (3) the lack of insulating snow cover during freezing temperatures, resulting in increased frost and decreased temperatures in soil. Meteorological records were used to define variables describing the conditions of each hypothesis and a dynamic frost hardiness model was used to find events of insufficient frost hardiness levels. As frost damage is likely to occur only under exceptional conditions, we used generalized extreme value distributions to describe the frost variables. Our results did not show strong connections between radial growth and the frost damage events. However, significant growth reductions were found at some Norway spruce sites after events insufficient frost hardiness levels, and alternatively, after winters with high frost sum of snowless days. Scots pine did not show significant growth reductions associated with any of the studied variables. Thus, radial growth in Norway spruce may be more sensitive to future changes in winter conditions. Our results demonstrate that considering only temperature is unlikely to be sufficient in studying winter temperature effects on tree growth. Instead, understanding the effects of changing temperature and snow conditions in relation to tree physiology and phenology is needed.

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  • 21 September 2017

    In the original publication the captions of Figs. 7 and 8 had unfortunately been swapped. The correct figure captions are given below:

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Acknowledgements

The study was conducted in the Natural Resources Institute Finland. The work was supported by grants from the Academy of Finland (Nos. 257641, 265504 and 288267). We thank Achim Drebs from the Finnish Meteorological Institute for providing us with pre-1960s weather data.

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Correspondence to Susanne Suvanto.

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Communicated by T. Kajimoto.

An erratum to this article is available at https://doi.org/10.1007/s00468-017-1617-4.

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Suvanto, S., Henttonen, H.M., Nöjd, P. et al. Connecting potential frost damage events identified from meteorological records to radial growth variation in Norway spruce and Scots pine. Trees 31, 2023–2034 (2017). https://doi.org/10.1007/s00468-017-1590-y

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