Reconstructing the time history of the air-sea CO2 disequilibrium and its rate of change in the eastern subpolar North Atlantic, 1972–1989
Peer reviewed, Journal article
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- Geophysical Institute 
Original versionGeophysical research letters 2006 33(4) https://doi.org/10.1029/2005gl025425
This study determines the temporal changes of wintertime surface ocean partial pressure of CO2 (pCO2 SW) in the eastern subpolar North Atlantic (esNA) (50–64ºN; 32–10ºW) by using data of carbon-system parameters and chlorofluorocarbon-12 acquired in 1993. Wintertime pCO2 SW and its temporal trend from early 1970s through to the late 1980s were reconstructed through the application of a back-calculation method that isolates surface variations which have been transmitted to the ocean interior during the formation of Subpolar Mode Water. Our computations suggest a pCO2 SW growth rate (3 matm/yr) which is twice as large as that of atmospheric pCO2, 1.47 matm/yr. The sensitivity of the estimated pCO2 SW growth rate to remineralization ratios as well as to the CFC-12-derived ages is discussed. Cooling and northward advection of surface water equilibrated with the increasing atmospheric CO2 is suggested as the process responsible for the excessive pCO2 SW growth rate.