No Future Growth Enhancement Expected at the Northern Edge for European Beech due to Continued Water Limitation

50+1, Stefan Klesse*, Richard L. Peters, Raquel Alfaro-Sánchez, Vincent Badeau, Claudia Baittinger, Giovanna Battipaglia, Didier Bert, Franco Biondi, Michal Bosela, Marius Budeanu, Vojtěch Čada, J. Julio Camarero, Liam Cavin, Hugues Claessens, Ana-Maria Cretan, Katarina Čufar, Martin de Luis, Isabel Dorado-Liñán, Choimaa DulamsurenJosep Maria Espelta, Balazs Garamszegi, Michael Grabner, Jozica Gricar, Andrew Hacket-Pain, Jon Kehlet Hansen, Claudia Hartl, Andrea Hevia, Martina Hobi, Pavel Janda, Alistair S. Jump, Jakub Kašpar, Marko Kazimirović, Srdjan Keren, Juergen Kreyling, Alexander Land, Nicolas Latte, François Lebourgeois, Christoph Leuschner, Mathieu Lévesque, Luis A. Longares, Edurne Martinez del Castillo, Annette Menzel, Maks Merela, Martin Mikoláš, Renzo Motta, Lena Muffler, Anna Neycken, Paola Nola, Momchil Panayotov, Any Mary Petritan

*Corresponding author for this work

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Abstract

With ongoing global warming, increasing water deficits promote physiological stress on forest ecosystems with negative impacts on tree growth, vitality, and survival. How individual tree species will react to increased drought stress is therefore a key research question to address for carbon accounting and the development of climate change mitigation strategies. Recent tree-ring studies have shown that trees at higher latitudes will benefit from warmer temperatures, yet this is likely highly species-dependent and less well-known for more temperate tree species. Using a unique pan-European tree-ring network of 26,430 European beech (Fagus sylvatica L.) trees from 2118 sites, we applied a linear mixed-effects modeling framework to (i) explain variation in climate-dependent growth and (ii) project growth for the near future (2021–2050) across the entire distribution of beech. We modeled the spatial pattern of radial growth responses to annually varying climate as a function of mean climate conditions (mean annual temperature, mean annual climatic water balance, and continentality). Over the calibration period (1952–2011), the model yielded high regional explanatory power (R2 = 0.38–0.72). Considering a moderate climate change scenario (CMIP6 SSP2-4.5), beech growth is projected to decrease in the future across most of its distribution range. In particular, projected growth decreases by 12%–18% (interquartile range) in northwestern Central Europe and by 11%–21% in the Mediterranean region. In contrast, climate-driven growth increases are limited to around 13% of the current occurrence, where the historical mean annual temperature was below ~6°C. More specifically, the model predicts a 3%–24% growth increase in the high-elevation clusters of the Alps and Carpathian Arc. Notably, we find little potential for future growth increases (−10 to +2%) at the poleward leading edge in southern Scandinavia. Because in this region beech growth is found to be primarily water-limited, a northward shift in its distributional range will be constrained by water availability.
Original languageEnglish
Article numbere17546
JournalGlobal change biology
Volume30
Issue number10
Number of pages16
ISSN1354-1013
DOIs
Publication statusPublished - 2024

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