Variability of the ocean carbon cycle in response to the North Atlantic Oscillation

Kathrin M. Keller (1, 2) , Fortunat Joos (1, 2) , Christoph C. Raible (1, 2) , Valentina Cocco (1, 2) , Thomas L. Frölicher (3) , John P. Dunne (4) , Marion Gehlen (5, 6) , Laurent Bopp (5) , James C. Orr (5, 6) , Jerry Tjiputra (7, 8) , Christoph Heinze (7, 8) , Joachim Segschneider (9) , Tilla Roy (10) , Nicolas Metzl (11, 12)

1 CEP - Climate and Environmental Physics [Bern]
2 OCCR - Oeschger Centre for Climate Change Research
3 AOS Program - Atmospheric and Oceanic Sciences Program [Princeton]
4 GFDL - NOAA Geophysical Fluid Dynamics Laboratory
5 LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
6 MERMAID - Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics
7 Uni Research Climate
8 BCCR - Bjerknes Centre for Climate Research
9 MPI-M - Max-Planck-Institut für Meteorologie
10 LOCEAN - Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques
11 PHYBIOCAR - Couplage physique-biogéochimie-carbone
12 E-CO2 - Équipe CO2

Climate modes such as the North Atlantic Oscillation (NAO), representing internal variability of the climate system, influence the ocean carbon cycle and may mask trends in the sink of anthropogenic carbon. Here, utilising control runs of six fully coupled Earth System Models, the response of the ocean carbon cycle to the NAO is quantified. The dominating response, a seesaw pattern between the subtropical gyre and the subpolar Northern Atlantic, is instantaneous (<3 months) and dynamically consistent over all models and with observations for a range of physical and biogeochemical variables. All models show asymmetric responses to NAO+ and NAO− forcing, implying non-linearity in the connection between NAO and the ocean carbon cycle. However, model differences in regional expression and magnitude and conflicting results with regard to air–sea flux and CO2 partial pressure remain. Typical NAO-driven variations are ±10 mmol/m3 in the surface concentration of dissolved inorganic carbon and alkalinity and ±8 ppm in the air–sea partial pressure difference. The effect on the basin-wide air–sea CO2 flux is small due to compensating fluxes on the sub-basin scale. Two models show a reduced carbon sink in the north-eastern North Atlantic during negative NAO phases, qualitatively in accordance with the observed decline during a phase of predominantly negative NAO. The results indicate that wind-driven dynamics are the main driver of the response to the NAO, which – via vertical mixing, upwelling and the associated entrainment of dissolved inorganic carbon and nutrients – leave an imprint on surface pCO2 and the air–sea CO2 flux as well as on biological export production, pH and the calcium carbonate saturation state. The biogeochemical response to the NAO is predominantly governed by vertical exchange between the surface and the thermocline; large-scale horizontal transport mechanisms are of minor importance

Mots clés: carbon cycle; ocean biogeochemistry; climate modeling; ocean-atmosphere interaction

Domaines: Océan, Atmosphère; Océanographie

Kathrin M. Keller, Fortunat Joos, Christoph C. Raible, Valentina Cocco, Thomas L. Frölicher, et al.. Variability of the ocean carbon cycle in response to the North Atlantic Oscillation. Tellus B - Chemical and Physical Meteorology, 2012, 64 (1), pp.18738. ⟨10.3402/tellusb.v64i0.18738⟩. ⟨hal-01111200⟩