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Systematic study of the impact of fresh water fluxes on the glacial carbon cycle

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Academic year: 2021

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Fig. 1. Evolution of the fresh water flux (Sv) in the three types of experiments: (a) for the “Duration” experiments with fresh water fluxes of 0.2 Sv added during 400, 700, 1100 or 1700 yr, (b) for the
Fig. 2. Evolution of (a, b, c) NADW export (Sv) (maximum of the AMOC), (d, e, f) atmospheric CO 2 (ppm), (g, h, i) carbon content anomaly in the terrestrial biosphere (GtC) and (j, k, l) carbon content anomaly in the ocean (GtC) during the simulations with
Fig. 3. Temperature and precipitation change. (a) Air temperature ( ◦ C) and (b) precipitation (mm yr −1 ) anomalies for the simulation during the Preindustrial with a fresh water flux added in the North Atlantic of 0.5 Sv during 400 yr
Fig. 4. Zonally averaged salinity (permil) and temperature ( ◦ C) anomalies, and density (kg m −3 ) for the simulation during the Preindustrial with a fresh water flux added in the North Atlantic of 0.5 Sv during 400 yr: (a, b, c) salinity; (d, e, f) tempe
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