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Climate-induced oceanic oxygen fluxes: Implications for the contemporary carbon budget

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Academic year: 2021

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Figure 4. Annual mean O 2 fluxes (mol m 2 yr 1 ) for first 100 years of simulation (1860 – 1960)
Figure 7. Total heat content of the ocean (10 22 J) integrated (a) from 0 to 300 m and (b) from 0 to 3000 m for 1950 – 2000 period.
Figure 9. Climate change impact (difference between 2080 – 2100 and 1980 – 2000) on (a) O 2 fluxes (mol m 2 yr 1 ), (b) sea surface temperature (SST) (C), (c) mixed layer depth (m), and (d) export production (g C m 2 yr 1 ).
Figure 12. Scatterplot of O *(mmol L 2 1 ) versus q (C) for (a) observations [Levitus and Boyer, 1994; Conkright et al., 1994], (b) model results for 1980 – 2000, and (c) model results for 2080 – 2100
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