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Table 1.

The zonally integrated future (2010–2100) cumulated CO2 uptake (PgC) due to rising atmospheric CO2 concentrations (ΔCCO2). The regional CO2 uptakes are listed in parentheses as a percentage of the global cumulated CO2 uptake. A positive cumulated CO2 uptake is a flux of atmospheric CO2 into the ocean.

The zonally integrated future (2010–2100) cumulated CO2 uptake (PgC) due to rising atmospheric CO2 concentrations (ΔCCO2). The regional CO2 uptakes are listed in parentheses as a percentage of the global cumulated CO2 uptake. A positive cumulated CO2 uptake is a flux of atmospheric CO2 into the ocean.
The zonally integrated future (2010–2100) cumulated CO2 uptake (PgC) due to rising atmospheric CO2 concentrations (ΔCCO2). The regional CO2 uptakes are listed in parentheses as a percentage of the global cumulated CO2 uptake. A positive cumulated CO2 uptake is a flux of atmospheric CO2 into the ocean.
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