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Air-sea gas exchange is a physico-chemical process, primarily controlled by the air-sea
difference in gas concentrations and the exchange coefficient, which determines how
quickly a molecule of gas can move across the ocean-atmosphere boundary. It takes about
one year to equilibrate CO
2 in the surface ocean with atmospheric
CO
2, so it is not unusual to observe large air-sea differences in
CO
2 concentrations. Most of the differences are caused by
variability in the oceans due to biology and ocean circulation. The oceans contain a very
large reservoir of carbon that can be exchanged with the atmosphere because the
CO
2 reacts with water to form carbonic acid and its
dissociation products. As atmospheric CO
2 increases in the future,
the interaction with the surface ocean will change the chemistry of the seawater.
The total dissolved inorganic carbon (DIC)
content of the waters will increase. Because CO
2 is an acid gas,
the carbonate ion (CO
32-) concentration
and pH of the surface waters will decrease.
The physiological effects of these changes on ocean biology are not fully understood,
but studies have suggested
that these changes may decrease calcification rates in coccoliths, corals, and coralline algae.
The PMEL carbon group participates in a growing network of
surface ocean observations
aimed at monitoring and evaluating the surface ocean CO
2
changes and understanding the potential environmental consequences of these changes.
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