Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/59587
Title: Spatial variability and temporal trends in water-use efficiency of European forests
Author: Saurer, M.
Spahni, R.
Frank, D.
Joos, F.
Leuenberger, M.
Loader, N.
McCarroll, D.
Gagen, M.
Poulter, B.
Siegwolf, R.
Andreu-Hayles, L.
Boettger, T.
Dorado Liñán, Isabel
Fairchild, I.
Friedrich, M.l
Gutiérrez Merino, Emilia
Haupt, M.
Hilasvuori, E.
Heinrich, I.
Helle, G.
Grudd, H.
Jalkanen, R.
Levanic, T.
Linderholm, H.
Robertson, I.
Sonninen, E.
Treydt, K.
Waterhouse, J.
Woodley, E.
Wynn, P.
Young, G.
Keywords: Boscos
Climatologia
Canvis climàtics
Dendrocronologia
Europa
Forests
Climatology
Climatic changes
Dendrochronology
Europe
Issue Date: 22-Aug-2014
Publisher: John Wiley & Sons
Abstract: 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<br>2000. The results were compared with simulations of a dynamic vegetation model (LPX-Bern 1.0) that integrates numerous ecosystem and land<br>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 strongest increase 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 of iWUE. These findings will help to reduce uncertainties in the land surface schemes of global climate models, where vegetation<br>climate feedbacks are currently still poorly constrained by observational data.
Note: Versió postprint del document publicat a: http://dx.doi.org/10.1111/gcb.12717
It is part of: Global Change Biology, 2014, vol. 20, num. 12, p. 3700-3712
Related resource: http://dx.doi.org/10.1111/gcb.12717
URI: http://hdl.handle.net/2445/59587
ISSN: 1354-1013
Appears in Collections:Articles publicats en revistes (Biologia Evolutiva, Ecologia i Ciències Ambientals)

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