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Dynamical and biogeochemical control on the decadal variability of ocean carbon fluxes

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Academic year: 2021

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Fig. 1. Long-term mean of (a) simulated ocean carbon fluxes (in g C m −2 yr −1 ) and (b) simulated regional carbon fluxes (in Pg C yr −1 ) compared to inversion-based estimates published in Mikaloff Fletcher et al
Fig. 2. Interannual time-series of the drift-corrected globally integrated ocean carbon flux (in Pg C yr −1 ) is represented in (a)
Fig. 3. Regional variability of (a) the ocean carbon uptake (in Pg C yr −1 ) and the area-weighted carbon fluxes (in g C m −2 yr −1 ) at (b) 1 yr (interannual), 5-, 10- and 20 yr time-scales
Fig. 4. Scaled spectral density of the five leading principal components of ocean carbon fluxes for (a) the North Atlantic (10 ◦ N–80 ◦ N), (b) the North Pacific (10 ◦ N–70 ◦ N) and (c) the Southern ocean(< 50 ◦ S)
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