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Nat Commun. 2016 Jan 18;7:10315. doi: 10.1038/ncomms10315.

European land CO2 sink influenced by NAO and East-Atlantic Pattern coupling.

Nature communications

Ana Bastos, Ivan A Janssens, Célia M Gouveia, Ricardo M Trigo, Philippe Ciais, Frédéric Chevallier, Josep Peñuelas, Christian Rödenbeck, Shilong Piao, Pierre Friedlingstein, Steven W Running

Affiliations

  1. Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, F-91191 Gif-sur-Yvette, France.
  2. Instituto Dom Luiz, IDL, Faculdade de Ciências, Universidade de Lisboa, Lisboa 1749-016, Portugal.
  3. Department of Biology, University of Antwerp, Universiteitsplein 1, 2610 Wilrijk, Belgium.
  4. CREAF, Cerdanyola del Vallès, Catalonia, 08193 Barcelona, Spain.
  5. CSIC, Global Ecology Unit CREAF-CSIC-UAB, Cerdanyola del Vallès, Catalonia, 08193 Barcelona, Spain.
  6. Max Planck Institute for Biogeochemistry, Jena 07701, Germany.
  7. Department of Ecology, College of Urban and Environmental Sciences, Peking University 5 Yiheyuan Road, Haidian District, Beijing 100871, China.
  8. College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QF, UK.
  9. Numerical Terradynamic Simulation Group, University of Montana, Missoula, Montana 59812, USA.

PMID: 26777730 PMCID: PMC4735626 DOI: 10.1038/ncomms10315

Abstract

Large-scale climate patterns control variability in the global carbon sink. In Europe, the North-Atlantic Oscillation (NAO) influences vegetation activity, however the East-Atlantic (EA) pattern is known to modulate NAO strength and location. Using observation-driven and modelled data sets, we show that multi-annual variability patterns of European Net Biome Productivity (NBP) are linked to anomalies in heat and water transport controlled by the NAO-EA interplay. Enhanced NBP occurs when NAO and EA are both in negative phase, associated with cool summers with wet soils which enhance photosynthesis. During anti-phase periods, NBP is reduced through distinct impacts of climate anomalies in photosynthesis and respiration. The predominance of anti-phase years in the early 2000s may explain the European-wide reduction of carbon uptake during this period, reported in previous studies. Results show that improving the capability of simulating atmospheric circulation patterns may better constrain regional carbon sink variability in coupled carbon-climate models.

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