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Research Article

Selected breakpoints of net forest carbon uptake at four eddy-covariance sites

ORCID Icon, , ORCID Icon, ORCID Icon, ORCID Icon & ORCID Icon
Pages 1-12 | Received 24 Mar 2020, Accepted 08 Apr 2021, Published online: 04 May 2021
 

Abstract

Extensive studies are available that analyse time series of carbon dioxide and water flux measurements of FLUXNET sites over many years and link these results to climate change such as changes in atmospheric carbon dioxide concentration, air temperature and growing season length and other factors. Many of the sites show trends to a larger carbon uptake. Here we analyse time series of net ecosystem exchange, gross primary production, respiration, and evapotranspiration of four forest sites with particularly long measurement periods of about 20 years. The regular trends shown are interrupted by periods with higher or lower increases of carbon uptake. These breakpoints can be of very different origin and include forest decline, increased vegetation period, drought effects, heat waves, and changes in site heterogeneity. The influence of such breakpoints should be included in long-term studies of land-atmosphere exchange processes.

Disclosure statement

No potential conflict of interest was reported by the authors.

Supplementary data

The data of DE-Bay site are available in Foken (Citation2017), https://link.springer.com/content/pdf/bbm%3A978-3-319-49389-3%2F1.pdf, and the data of the other sites on the data portal serving the FLUXNET community (https://fluxnet.fluxdata.org).

Additional information

Funding

The Hainich site was funded by the European Community (CARBOEUROFLUX), the Max-Planck Society, the Federal Ministry of Education, Science, Research and Technology, the German Science Foundation (INST 186/1118-1 FUGG) , and is currently funded by the University of Göttingen. The operation of the Waldstein-Weidenbrunnen site was funded by The Federal Ministry of Education, Science, Research and Technology (PT BEO-0339476 B, C, D), the European Community (EUROFLUX), the German Science Foundation (FO 226/16-1, FO 226/22-1), and the Oberfranken Foundation (contract 01879). The financial support by the Academy of Finland Centre of Excellence (118780), Academy Professor projects (312571 and 282842), and ICOS-Finland (319871) are acknowledged.