Preprints
https://doi.org/10.5194/egusphere-2025-2361
https://doi.org/10.5194/egusphere-2025-2361
30 May 2025
 | 30 May 2025
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Unpacking climate effects on boreal tree growth: An analysis of tree-ring widths across temperature and soil moisture gradients

Andreas Lundgren, Joachim Strengbom, Johannes Edvardsson, and Gustaf Granath

Abstract. The effect of climate change on tree growth in boreal forests is likely mediated by local climate conditions and species-specific responses that vary according to differences in traits. Here, we assess species-specific tree growth responses to climate along gradients of mean annual temperature (MAT) and soil moisture (SMI).

We assessed growth-climate relationships by using tree-ring width data in Norway spruce (Picea abies) and Scots pine (Pinus sylvestris) from the Swedish National Forest Inventory in relation to climatological data along MAT and SMI gradients.

Trees growing in warmer areas responded more negatively to high temperature and more positively to high precipitation. Site-specific SMI only showed an effect on the growth responses in areas of high MAT. The growth-climate response differed between the species; specifically, the growth response to high temperature varied more along the MAT gradient for P. abies than for P. sylvestris. Growth responses to extreme weather events did not deviate from non-extreme events along the climatic gradients.

Our study suggests that tree growth responses to climate change will depend on tree species, and that the response will be more sensitive to site-specific temperature variations than to local soil moisture conditions. High soil moisture may mitigate the adverse effects of climate change on tree growth in areas with a high mean annual temperature. Although the matching between extreme tree growth and extreme temperature or precipitation years was consistently higher than expected if the two variables were independent, an extreme year is unlikely to cause a tree growth response that markedly diverges from predictions based on linear relationships. Thus, the amplification of negative growth-climate responses during extreme years is likely of limited importance for long-term growth, as such events are inherently rare. However, extreme years may still significantly impact forest productivity by influencing tree mortality, which was beyond the scope of this study. In the face of climate change, forest management should consider site-specific climate conditions and species differences to sustain future forest productivity.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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Andreas Lundgren, Joachim Strengbom, Johannes Edvardsson, and Gustaf Granath

Status: open (until 24 Jul 2025)

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  • RC1: 'Comment on egusphere-2025-2361', Eric Gustafson, 13 Jun 2025 reply
Andreas Lundgren, Joachim Strengbom, Johannes Edvardsson, and Gustaf Granath

Data sets

Dataset for "Unpacking climate effects on boreal tree growth: An analysis of tree-ring widths across temperature and soil moisture gradients". Lundgren, A., Strengbom, J., Edvardsson, J., Granath, G. https://doi.org/10.5281/zenodo.12655494

Model code and software

Project_GeoTree Lundgren, A. https://github.com/LundgrenAndreas/Research/tree/main/Project_GeoTree

Andreas Lundgren, Joachim Strengbom, Johannes Edvardsson, and Gustaf Granath

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Short summary
By studying tree-rings and climatic data throughout Sweden, we have found that tree-growth in warm areas is more negatively affected by increasing temperature than tree-growth in cold areas. We also found that soil moisture has a very small effect when it comes to mitigating the negative effect of increasing temperature. These findings suggest that tree-growth responses to a changing climate will likely vary with the local climate but not so much with differences in soil moisture.
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