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Khatiwala, S.; Tanhua, T.; Mikaloff Fletcher, S.; Gerber, M.; Doney, S. C.; Graven, H. D.; Gruber, N.; McKinley, G. A.; Murata, A.; Ríos, A. F.; Sabine, C. L.; Sarmiento, J. L. (2012)
Publisher: Copernicus Publications
Journal: Biogeosciences Discussions
Types: Article
Subjects: DOAJ:Earth and Environmental Sciences, DOAJ:Earth Sciences, QH540-549.5, QE1-996.5, Evolution, QH501-531, Geology, DOAJ:Biology, Life, QH301-705.5, Q, Ecology, Science, 530 Physics, DOAJ:Biology and Life Sciences, QH359-425, Biology (General)
The global ocean is a significant sink for anthropogenic carbon (C<sub>ant</sub>), absorbing roughly a third of human CO<sub>2</sub> emitted over the industrial period. Robust estimates of the magnitude and variability of the storage and distribution of C<sub>ant</sub> in the ocean are therefore important for understanding the human impact on climate. In this synthesis we review observational and model-based estimates of the storage and transport of C<sub>ant</sub> in the ocean. We pay particular attention to the uncertainties and potential biases inherent in different inference schemes. On a global scale, three data based estimates of the distribution and inventory of C<sub>ant</sub> are now available. While the inventories are found to agree within their uncertainty, there are considerable differences in the spatial distribution. We also present a review of the progress made in the application of inverse and data-assimilation techniques which combine ocean interior estimates of C<sub>ant</sub> with numerical ocean circulation models. Such methods are especially useful for estimating the air-sea flux and interior transport of C<sub>ant</sub>, quantities that are otherwise difficult to observe directly. However, the results are found to be highly dependent on modeled circulation, with the spread due to different ocean models at least as large as that from the different observational methods used to estimate C<sub>ant</sub>. Our review also highlights the importance of repeat measurements of hydrographic and biogeochemical parameters to estimate the storage of C<sub>ant</sub> on decadal timescales in the presence of the variability in circulation that is neglected by other approaches. Data-based C<sub>ant</sub> estimates provide important constraints on ocean forward models, which exhibit both broad similarities and regional errors relative to the observational fields. A compilation of inventories of C<sub>ant</sub> gives us a "best" estimate of the global ocean inventory of anthropogenic carbon in 2010 of 155 Pg C with an uncertainty of ±20%. This estimate includes a broad range of values suggesting that a combination of approaches is necessary in order to achieve a robust quantification of the ocean sink of anthropogenic CO<sub>2</sub>.

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