Observation-based trends of the southern ocean carbon sink

Ritter, R.; Landschützer, Peter; Gruber, N.; Fay, A. R.; Iida, Y.; Jones, S.; Nakaoka, S.; Park, G. -H.; Peylin, P.; Rödenbeck, C.; Rodgers, K. B.; Shutler, J. D.; Zeng, J.

doi:10.1002/2017GL074837

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Observation-based trends of the southern ocean carbon sink

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Landschützer, Peter
Director’s Research Group OES, The Ocean in the Earth System, MPI for Meteorology, Max Planck Society;

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Ritter_et_al-2017-Geophysical_Research_Letters.pdf
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引用

Ritter, R., Landschützer, P., Gruber, N., Fay, A. R., Iida, Y., Jones, S., Nakaoka, S., Park, G.-.-H., Peylin, P., Rödenbeck, C., Rodgers, K. B., Shutler, J. D., & Zeng, J. (2017). Observation-based trends of the southern ocean carbon sink. Geophysical Research Letters, 44, 12,339-12,348. doi:10.1002/2017GL074837.

引用: https://hdl.handle.net/11858/00-001M-0000-002E-A0CE-3

要旨

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.