Articles | Volume 14, issue 12
https://doi.org/10.5194/bg-14-3083-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-3083-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Tree growth and its climate signal along latitudinal and altitudinal gradients: comparison of tree rings between Finland and the Tibetan Plateau
State Key Laboratory of Vegetation and Environmental Change, Institute
of Botany, Chinese Academy of Sciences, Beijing, 100093, China
Susanne Suvanto
Natural Resources Institute Finland, Bio-Based Business and Industry,
c/o Aalto University, P.O. Box 16200, 00076 Espoo, Finland
Pekka Nöjd
Natural Resources Institute Finland, Bio-Based Business and Industry,
c/o Aalto University, P.O. Box 16200, 00076 Espoo, Finland
Helena M. Henttonen
Natural Resources Institute Finland, Economics and Society, P.O. Box 2,
00791 Helsinki, Finland
Harri Mäkinen
Natural Resources Institute Finland, Bio-Based Business and Industry,
c/o Aalto University, P.O. Box 16200, 00076 Espoo, Finland
Qi-Bin Zhang
State Key Laboratory of Vegetation and Environmental Change, Institute
of Botany, Chinese Academy of Sciences, Beijing, 100093, China
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- Variability in radial increment can predict an abrupt decrease in tree growth during forest decline: Tree-ring patterns of Abies alba Mill. in near-natural forests R. Podlaski 10.1016/j.foreco.2020.118579
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- A Tree-Ring-Based Assessment of Pinus armandii Adaptability to Climate Using Two Statistical Methods in Mt. Yao, Central China during 1961–2016 J. Peng et al. 10.3390/f12060780
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Latest update: 14 Dec 2024
Short summary
Our results reveal that the change in the tree growth–climate relationship is similar along latitudinal and altitudinal gradients, especially during growing seasons. Moreover, the critical periods for climatic effects on tree radial growth occurred earlier at lower latitudes and altitudes than at the cold ends of the gradients. We further demonstrate the use of daily climate data, as they may disclose more precise gradient patterns that could not be detected if monthly climate data were used.
Our results reveal that the change in the tree growth–climate relationship is similar along...
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