Carbonate system distribution, anthropogenic carbon and acidification in the western tropical South Pacific (OUTPACE 2015 transect)

The western tropical South Pacific was sampled along a longitudinal 4000 km transect (OUTPACE cruise, 18 February, 3 April 2015) for the measurement of carbonate parameters (total alkalinity and total inorganic carbon) between the Melanesian Archipelago (MA) and the western part of the South Pacific...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Wagener, Thibaut, Metzl, Nicolas, Caffin, Mathieu, Fin, Jonathan, Helias Nunige, Sandra, Lefevre, Dominique, Lo Monaco, Claire, Rougier, Gilles, Moutin, Thierry
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
article
Verlagsveröffentlichung
Pacific
Ocean acidification
Online Access:https://doi.org/10.5194/bg-15-5221-2018
https://noa.gwlb.de/receive/cop_mods_00004984
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00004941/bg-15-5221-2018.pdf
https://bg.copernicus.org/articles/15/5221/2018/bg-15-5221-2018.pdf
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Summary:The western tropical South Pacific was sampled along a longitudinal 4000 km transect (OUTPACE cruise, 18 February, 3 April 2015) for the measurement of carbonate parameters (total alkalinity and total inorganic carbon) between the Melanesian Archipelago (MA) and the western part of the South Pacific gyre (WGY). This paper reports this new dataset and derived properties: pH on the total scale (pHT) and the CaCO3 saturation state with respect to aragonite (Ωara). We also estimate anthropogenic carbon (CANT) distribution in the water column using the TrOCA method (Tracer combining Oxygen, inorganic Carbon and total Alkalinity). Along the OUTPACE transect a deeper penetration of CANT in the intermediate waters was observed in the MA, whereas highest CANT concentrations were detected in the subsurface waters of the WGY. By combining our OUTPACE dataset with data available in GLODAPv2 (1974–2009), temporal changes in oceanic inorganic carbon were evaluated. An increase of 1.3 to 1.6 µmol kg−1 a−1 for total inorganic carbon in the upper thermocline waters is estimated, whereas CANT increases by 1.1 to 1.2 µmol kg−1 a−1. In the MA intermediate waters (27 kg m−3 <σθ<27.2 kg m−3) an increase of 0.4 µmol kg−1 a−1 CANT is detected. Our results suggest a clear progression of ocean acidification in the western tropical South Pacific with a decrease in the oceanic pHT of up to −0.0027 a−1 and a shoaling of the saturation depth for aragonite of up to 200 m since the pre-industrial period.

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