Global ocean carbon uptake: magnitude, variability and trends

TitleGlobal ocean carbon uptake: magnitude, variability and trends
Publication TypeJournal Article
Year of Publication2013
AuthorsWanninkhof R, Park GH, Takahashi T, Sweeney C, Feely R, Nojiri Y, Gruber N, Doney SC, McKinley GA, Lenton A, Le Quere C, Heinze C, Schwinger J, Graven H, Khatiwala S
JournalBiogeosciences
Volume10
Pagination1983-2000
Date Published2013/03
Type of ArticleArticle
ISBN Number1726-4170
Accession NumberWOS:000317010600048
Keywordsair co2 fluxes; atmospheric co2; climate-change; dioxide; interannual; north-atlantic; sampling-network; sea gas-exchange; sinks; variability; wind-speed
Abstract

The globally integrated sea-air anthropogenic carbon dioxide (CO2) flux from 1990 to 2009r is determined from models and data-based approaches as part of the Regional Carbon Cycle Assessment and Processes (RECCAP) project. Numerical methods include ocean inverse models, atmospheric inverse models, and ocean general circulation models with parameterized biogeochemistry (OBGCMs). The median value of different approaches shows good agreement in average uptake. The best estimate of anthropogenic CO2 uptake for the time period based on a compilation of approaches is -2.0 PgC yr(-1). The interannual variability in the sea-air flux is largely driven by large-scale climate re-organizations and is estimated at 0.2 Pg C yr(-1) for the two decades with some systematic differences between approaches. The largest differences between approaches are seen in the decadal trends. The trends range from -0.13 (Pg C yr(-1)) decade(-1) to -0.50 (Pg C yr(-1)) decade(-1) for the two decades under investigation. The OBGCMs and the data-based sea-air CO2 flux estimates show appreciably smaller decadal trends than estimates based on changes in carbon inventory suggesting that methods capable of resolving shorter timescales are showing a slowing of the rate of ocean CO2 uptake. RECCAP model outputs for five decades show similar differences in trends between approaches.

DOI10.5194/bg-10-1983-2013
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