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A multi-decadal delay in the onset of corrosive ‘acidified’ waters in the Ross Sea of Antarctica due to strong air-sea CO 2 disequilibrium

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Academic year: 2021

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Table 1. Average Values of Physical and Chemical Properties for Water Masses Found in the Ross Sea a
Figure 3. (a) Atmospheric CO 2 scenario (IPCC is92a) used in the model analysis. (b) Winter‐time anthropogenic CO 2 storage (mmol/kg) between 1997 and 2020 at a specific location in the central Ross Sea (76.5°S, 177°E) simulated using a three‐dimensional r
Figure 4. Equilibrium and dis‐equilibrium projections of winter ‐ time Aragonite Saturation State ( W ARAG ) from 1997 to the year 2050 under the IPCC IS92a atmospheric CO 2 scenario for the Ross Sea

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