TY - JOUR
T1 - No Future Growth Enhancement Expected at the Northern Edge for European Beech due to Continued Water Limitation
AU - 50+1
AU - Klesse, Stefan
AU - Peters, Richard L.
AU - Alfaro-Sánchez, Raquel
AU - Badeau, Vincent
AU - Baittinger, Claudia
AU - Battipaglia, Giovanna
AU - Bert, Didier
AU - Biondi, Franco
AU - Bosela, Michal
AU - Budeanu, Marius
AU - Čada, Vojtěch
AU - Camarero, J. Julio
AU - Cavin, Liam
AU - Claessens, Hugues
AU - Cretan, Ana-Maria
AU - Čufar, Katarina
AU - de Luis, Martin
AU - Dorado-Liñán, Isabel
AU - Dulamsuren, Choimaa
AU - Espelta, Josep Maria
AU - Garamszegi, Balazs
AU - Grabner, Michael
AU - Gricar, Jozica
AU - Hacket-Pain, Andrew
AU - Hansen, Jon Kehlet
AU - Hartl, Claudia
AU - Hevia, Andrea
AU - Hobi, Martina
AU - Janda, Pavel
AU - Jump, Alistair S.
AU - Kašpar, Jakub
AU - Kazimirović, Marko
AU - Keren, Srdjan
AU - Kreyling, Juergen
AU - Land, Alexander
AU - Latte, Nicolas
AU - Lebourgeois, François
AU - Leuschner, Christoph
AU - Lévesque, Mathieu
AU - Longares, Luis A.
AU - del Castillo, Edurne Martinez
AU - Menzel, Annette
AU - Merela, Maks
AU - Mikoláš, Martin
AU - Motta, Renzo
AU - Muffler, Lena
AU - Neycken, Anna
AU - Nola, Paola
AU - Panayotov, Momchil
AU - Petritan, Any Mary
PY - 2024
Y1 - 2024
N2 - 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.
AB - 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.
KW - climate change
KW - climate sensitivity
KW - drought
KW - Fagus sylvatica
KW - growth projection
KW - leading edge
KW - trailing edge
KW - tree rings
U2 - 10.1111/gcb.17546
DO - 10.1111/gcb.17546
M3 - Journal article
SN - 1354-1013
VL - 30
SP - e17546
JO - Global change biology
JF - Global change biology
IS - 10
ER -