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. 2013 Dec 5;27(4):1236–1245. doi: 10.1002/2013GB004600

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© 2013 The Authors. Global Biogeochemical Cycles published byWiley on behalf of the American Geophysical Union.

This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.

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The response of (as indicated in the figures) average SST, zonal velocity (u), and inventories in the 0–10 m layer of DFe, DSi, DIC, nanophytoplankton carbon biomass (C_phy), diatom carbon biomass (C_dia), total chlorophyll (Chl_tot), and the anomalous fluxes at 100 m for export production (C_exp), DFe (DFe_adv), DIC (C_adv), and CO₂ flux at the surface (C_gas-ex) plotted versus lags 0 to 12 months. Shown are the annual mean response (green), summer (red), and winter (blue) and the 95% confidence intervals of the regression south of 55°S.