Optimal evaluation of the surface ocean CO 2 system in the northern North Atlantic using data from voluntary observing ships

This work evaluates whether an accurate calculation of the entire CO 2 system in the northern North Atlantic can be carried out using a combination of in situ fugacity of CO 2 (fCO 2 ) and ancillary data often measured on Voluntary Observing Ships (VOS), i.e., sea surface temperature (SST) and sea s...

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Bibliographic Details
Published in:Limnology and Oceanography: Methods
Main Authors: Nondal, Gisle, Bellerby, Richard G. J., Olsen, Are, Johannessen, Truls, Olafsson, Jón
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
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Online Access:http://dx.doi.org/10.4319/lom.2009.7.109
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flom.2009.7.109
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lom.2009.7.109
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Summary:This work evaluates whether an accurate calculation of the entire CO 2 system in the northern North Atlantic can be carried out using a combination of in situ fugacity of CO 2 (fCO 2 ) and ancillary data often measured on Voluntary Observing Ships (VOS), i.e., sea surface temperature (SST) and sea surface salinity (SSS), as well as nitrate (NO 3 − ). Two approaches are tested: (I) determination of A t from SSS and then calculating C t from measured fCO 2 and estimated A t and (II) determination of C t from SSS, SST, and NO 3 − and then calculating A t from measured fCO 2 and estimated C t . The optimal approach was found to be determination of A t from SSS and then calculating C t from measured fCO 2 and estimated A t . This allowed A t to be determined with a mean bias of −1.8 µmol kg −1 and root mean square (rms) deviation 6.2 µmol kg −1 and then C t to be calculated with a mean bias of −1.0 µmol kg −1 and standard error of calculation of 7.4 µmol kg −1 , as validated using independent data sets.