Physical mechanisms for biological carbon uptake during the onset of the spring phytoplankton bloom in the northwestern mediterranean sea (boussole site)

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SUMMARY

L Merlivat et_al: Physical mechanisms for biological carbon uptake ent of CO2 partial pressure, pCO2, between the atmosphere and the surface ocean (Takahashi et_al, 2009; Rödenbeck et_al, 2013; Merlivat et_al, 2015). pCO2 in the ocean mixed surface layer depends on the relative contribution of dynamic transport, thermodynamics and biogeochemistry. The physical processes of wind stress, heat flux and vertical mixing control the depth of the mixed/mixing layer and thus the availability of light (Siegel et_al, 2002; Chiswell, 2011; Taylor and Ferrari, 2011; Brody and Lozier, 2015; Enriquez and Taylor, 2015; Rumyantseva et_al . . .

 



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