Final published version
Research output: Contribution to Journal/Magazine › Journal article › peer-review
Research output: Contribution to Journal/Magazine › Journal article › peer-review
}
TY - JOUR
T1 - Spatial variability and temporal trends in water‐use efficiency of European forests
AU - Saurer, Matthias
AU - Spahni, Renato
AU - Frank, David C.
AU - Joos, Fortunat
AU - Leuenberger, Markus
AU - Loader, Neil J.
AU - McCarroll, Danny
AU - Gagen, Mary
AU - Poulter, Benjamin
AU - Seigwolf, Rolf T. W.
AU - Andreu-Hayles, Laia
AU - Boettger, Tatjana
AU - Dorado Liñán, Isabel
AU - Fairchild, Ian J.
AU - Friedrich, Michael
AU - Gutierrez, Emilia
AU - Haupt, Marika
AU - Hilasvuori, Emmi
AU - Heinrich, Ingo
AU - Helle, Gerd
AU - Grudd, Håkan
AU - Jalkaen, Risto
AU - Levanič, Tom
AU - Linderholm, Hans W.
AU - Robertson, Iain
AU - Sonninen, Eloni
AU - Treydte, Kerstin
AU - Waterhouse, John S.
AU - Woodley, Ewan J.
AU - Wynn, Peter Michael
AU - Young, Giles H. F.
PY - 2014/12/1
Y1 - 2014/12/1
N2 - The increasing carbon dioxide (CO2) concentration in the atmosphere in combination with climatic changes throughout the last century are likely to have had a profound effect on the physiology of trees: altering the carbon and water fluxes passing through the stomatal pores. However, the magnitude and spatial patterns of such changes in natural forests remain highly uncertain.Here, stable carbon isotope ratios from a network of 35 tree-ring sites located across Europe are investigated to determine the intrinsic water-use efficiency (iWUE), the ratio of photosynthesis to stomatal conductance from 1901 to 2000. The results were compared with simulations of a dynamic vegetation model (LPX-Bern 1.0) that integrates numerous ecosystem and land–atmosphere exchange processes in a theoretical framework. The spatial pattern of tree-ring derived iWUE of the investigated coniferous and deciduous species and the model results agreed significantly with a clear south-to-north gradient, as well as a general increase in iWUE over the 20th century. The magnitude of the iWUE increase was not spatially uniform, with the strongestincrease observed and modelled for temperate forests in Central Europe, a region where summer soil-water availability decreased over the last century. We were able to demonstrate that the combined effects of increasing CO2 and climate change leading to soil drying have resulted in an accelerated increase in iWUE. These findings will help to reduce uncertainties in the land surface schemes of global climate models, where vegetation–climate feedbacks are currently still poorly constrained by observational data.
AB - The increasing carbon dioxide (CO2) concentration in the atmosphere in combination with climatic changes throughout the last century are likely to have had a profound effect on the physiology of trees: altering the carbon and water fluxes passing through the stomatal pores. However, the magnitude and spatial patterns of such changes in natural forests remain highly uncertain.Here, stable carbon isotope ratios from a network of 35 tree-ring sites located across Europe are investigated to determine the intrinsic water-use efficiency (iWUE), the ratio of photosynthesis to stomatal conductance from 1901 to 2000. The results were compared with simulations of a dynamic vegetation model (LPX-Bern 1.0) that integrates numerous ecosystem and land–atmosphere exchange processes in a theoretical framework. The spatial pattern of tree-ring derived iWUE of the investigated coniferous and deciduous species and the model results agreed significantly with a clear south-to-north gradient, as well as a general increase in iWUE over the 20th century. The magnitude of the iWUE increase was not spatially uniform, with the strongestincrease observed and modelled for temperate forests in Central Europe, a region where summer soil-water availability decreased over the last century. We were able to demonstrate that the combined effects of increasing CO2 and climate change leading to soil drying have resulted in an accelerated increase in iWUE. These findings will help to reduce uncertainties in the land surface schemes of global climate models, where vegetation–climate feedbacks are currently still poorly constrained by observational data.
KW - carbon isotope discrimination
KW - climate change
KW - dynamic vegetation model
KW - tree rings
U2 - 10.1111/gcb.12717
DO - 10.1111/gcb.12717
M3 - Journal article
VL - 20
SP - 3700
EP - 3712
JO - Global Change Biology
JF - Global Change Biology
SN - 1354-1013
IS - 12
ER -