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Contrasting effects of CO2 fertilization, land-use change and warming on seasonal amplitude of Northern Hemisphere CO2 exchange

  • Ana Bastos
  • , Philippe Ciais
  • , Frédéric Chevallier
  • , Christian Rödenbeck
  • , Ashley P. Ballantyne
  • , Fabienne Maignan
  • , Yi Yin
  • , Marcos Fernández-Martínez
  • , Pierre Friedlingstein
  • , Josep Peñuelas
  • , Shilong L. Piao
  • , Stephen Sitch
  • , William K. Smith
  • , Xuhui Wang
  • , Zaichun Zhu
  • , Vanessa Haverd
  • , Etsushi Kato
  • , Atul K. Jain
  • , Sebastian Lienert
  • , Danica Lombardozzi
  • Julia E.M.S. Nabel, Philippe Peylin, Benjamin Poulter, Dan Zhu
  • Ludwig Maximilian University of Munich
  • Université Paris-Saclay
  • Max Planck Institute for Biogeochemistry
  • California Institute of Technology
  • University of Antwerp
  • University of Exeter
  • CSIC
  • Centre de Recerca Ecològica i Aplicacions Forestals (CREAF)
  • Peking University
  • University of Arizona
  • CSIRO
  • The Institute of Applied Energy
  • University of Illinois at Urbana-Champaign
  • University of Bern
  • National Center for Atmospheric Research
  • Max Planck Institute for Meteorology
  • NASA Goddard Space Flight Center

Research output: Contribution to journalArticlepeer-review

45 Scopus citations

Abstract

Continuous atmospheric CO2 monitoring data indicate an increase in the amplitude of seasonal CO2-cycle exchange (SCANBP) in northern high latitudes. The major drivers of enhanced SCANBP remain unclear and intensely debated, with land-use change, CO2 fertilization and warming being identified as likely contributors. We integrated CO2-flux data from two atmospheric inversions (consistent with atmospheric records) and from 11 state-of-the-art land-surface models (LSMs) to evaluate the relative importance of individual contributors to trends and drivers of the SCANBP of CO2 fluxes for 1980-2015. The LSMs generally reproduce the latitudinal increase in SCANBP trends within the inversions range. Inversions and LSMs attribute SCANBP increase to boreal Asia and Europe due to enhanced vegetation productivity (in LSMs) and point to contrasting effects of CO2 fertilization (positive) and warming (negative) on SCANBP. Our results do not support land-use change as a key contributor to the increase in SCANBP. The sensitivity of simulated microbial respiration to temperature in LSMs explained biases in SCANBP trends, which suggests that SCANBP could help to constrain model turnover times.

Original languageEnglish
Article number652
Pages (from-to)12361-12375
Number of pages15
JournalAtmospheric Chemistry and Physics
Volume19
Issue number19
DOIs
StatePublished - Oct 7 2019

Funding

Acknowledgements. This work was partly supported by the European Space Agency Climate Change Initiative (ESA-CCI) RECCAP-2 project (ESRIN/ 4000123002/18/I-NB). Mar-cos Fernández-Martinez is a postdoctoral fellow of the Research Foundation – Flanders (FWO). Vanessa Haverd acknowledges support from the Earth Systems and Climate Change Hub, funded by the Australian government’s National Environmental Science Program. This work was partly supported by the European Space Agency Climate Change Initiative (ESACCI) RECCAP-2 project (ESRIN/ 4000123002/18/I-NB). Marcos Fern?ndez-Martinez is a postdoctoral fellow of the Research Foundation - Flanders (FWO). Vanessa Haverd acknowledges support from the Earth Systems and Climate Change Hub, funded by the Australian government's National Environmental Science Program.

Funder number
ESRIN/ 4000123002/18/I-NB

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 15 - Life on Land
      SDG 15 Life on Land

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