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Journal Article

Observation-based trends of the southern ocean carbon sink


Rödenbeck,  Christian
Inverse Data-driven Estimation, Dr. C. Rödenbeck, Department Biogeochemical Systems, Prof. M. Heimann, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Ritter, R., Landschützer, P., Gruber, N., Fay, A. R., Iida, Y., Jones, S., et al. (2017). Observation-based trends of the southern ocean carbon sink. Geophysical Research Letters, 44(24), 12339-12348. doi:10.1002/2017GL074837.

Cite as: https://hdl.handle.net/11858/00-001M-0000-002E-87FC-1
The Southern Ocean (SO) carbon sink has strengthened substantially since the year 2000, following a decade of a weakening trend. However, the surface ocean pCO2 data underlying this trend reversal are sparse, requiring a substantial amount of extrapolation to map the data. Here, we use 9 different pCO2 mapping products to investigate the SO trends and their sensitivity to the mapping procedure. We find a robust temporal coherence for the entire SO, with 8 of the 9 products agreeing on the sign of the decadal trends, i.e., a weakening CO2 sink trend in the in the 1990s (on average 0.22±0.24 Pg C yr−1 decade−1), and a strengthening sink trend during the 2000s (-0.35±0.23 Pg C yr−1 decade−1). Spatially, the multi-product mean reveals rather uniform trends, but the confidence is limited, given the small number of statistically significant trends from the individual products, particularly during the data sparse 1990-1999 period.