Decadal Trends in the Oceanic Storage of Anthropogenic Carbon From 1994 to 2014

• Main Authors: Müller, Jens Daniel, Gruber, Nicolas, Carter, Brendan R., Feely, Richard A., Ishii, Masao, Lange, Nico, Lauvset, Siv K., Murata, Akihiko, Olsen, Are, Pérez, Fiz F., Sabine, Christopher L., Tanhua, Toste, Wanninkhof, Rik, Zhu, Donghe
• Other Authors: European Commission, Ministerio de Ciencia e Innovación (España), Research Council of Norway, National Oceanic and Atmospheric Administration (US)
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union 2023
• Subjects: Norway; North Atlantic
• Online Access: http://hdl.handle.net/10261/333982; https://doi.org/10.1029/2023AV000875

28 pages, 2 tables, 8 figures.-- This is an open access article under the terms of the Creative Commons Attribution License The oceanic uptake and resulting storage of the anthropogenic CO2 (Cant) that humans have emitted into the atmosphere moderates climate change. Yet our knowledge about how this uptake and storage has progressed in time remained limited. Here, we determine decadal trends in the storage of Cant by applying, the eMLR(C*) regression method to ocean interior observations collected repeatedly since the 1990s. We find that the global ocean storage of Cant grew from 1994 to 2004 by 29 ± 3 Pg C dec−1 and from 2004 to 2014 by 27 ± 3 Pg C dec−1 (±1σ). The storage change in the second decade is about 15 ± 11% lower than one would expect from the first decade and assuming proportional increase with atmospheric CO2. We attribute this reduction in sensitivity to a decrease of the ocean buffer capacity and changes in ocean circulation. In the Atlantic Ocean, the maximum storage rate shifted from the Northern to the Southern Hemisphere, plausibly caused by a weaker formation rate of North Atlantic Deep Waters and an intensified ventilation of mode and intermediate waters in the Southern Hemisphere. Our estimates of the Cant accumulation differ from cumulative net air-sea flux estimates by several Pg C dec−1, suggesting a substantial and variable, but uncertain net loss of natural carbon from the ocean. Our findings indicate a considerable vulnerability of the ocean carbon sink to climate variability and change JDM and NG acknowledge support from the European Union's Horizon 2020 research and innovation programme under grant agreements no. 821003 (project 4C) and no. 821001 (SO-CHIC). FFP was supported by the BOCATS2 (PID2019-104279GB-C21) project funded by MCIN/AEI/10.13039/501100011033 and contributed to WATER:iOS CSIC PTI. AO and SKL were supported by the project N-ICOS-2 (Research Council of Norway Grant 296012). SKL also acknowledges internal funding support from NORCE. MI was supported by ...