4.7 Article

Quantifying the effect of forest age in annual net forest carbon balance

Journal

ENVIRONMENTAL RESEARCH LETTERS
Volume 13, Issue 12, Pages -

Publisher

IOP Publishing Ltd
DOI: 10.1088/1748-9326/aaeaeb

Keywords

carbon cycle; eddy covariance; net ecosystem production; empirical modelling; forest age; climate; soil properties

Funding

  1. US Department of Energy, Biological and Environmental Research, Terrestrial Carbon Program [DEFG0204ER63917, DEF-G0204ER63911]
  2. CFCAS
  3. NSERC
  4. BIO-CAP
  5. Environment Canada
  6. NRCan
  7. CarboEuropeIP
  8. FAOGTOSTCO
  9. iLEAPS
  10. Max Planck Institute for Biogeochemistry
  11. National Science Foundation
  12. University of Tuscia
  13. Universite Laval
  14. US Department of Energy
  15. BACI project
  16. Independent Monitoring Project
  17. Ministry of Education, Youth and Sports of the Czech Republic within the National Sustainability Programme I (NPU I) [LO1415]
  18. NOVA grant [UID/AMB/04085/2013]
  19. GlobBiomass project

Ask authors/readers for more resources

Forests dominate carbon (C) exchanges between the terrestrial biosphere and the atmosphere on land. In the long term, the net carbon flux between forests and the atmosphere has been significantly impacted by changes in forest cover area and structure due to ecological disturbances and management activities. Current empirical approaches for estimating net ecosystem productivity (NEP) rarely consider forest age as a predictor, which represents variation in physiological processes that can respond differently to environmental drivers, and regrowth following disturbance. Here, we conduct an observational synthesis to empirically determine to what extent climate, soil properties, nitrogen deposition, forest age and management influence the spatial and interannual variability of forest NEP across 126 forest eddy-covariance flux sites worldwide. The empirical models explained up to 62% and 71% of spatio-temporal and across-site variability of annual NEP, respectively. An investigation of model structures revealed that forest age was adominant factor of NEP spatio-temporal variability in both space and time at the global scale as compared to abiotic factors, such as nutrient availability, soil characteristics and climate. These findings emphasize the importance of forest age in quantifying spatio-temporal variation in NEP using empirical approaches.

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