Testing the climate intervention potential of ocean afforestation using the Great Atlantic Sargassum Belt

Abstract Ensuring that global warming remains <2 °C requires rapid CO 2 emissions reduction. Additionally, 100–900 gigatons CO 2 must be removed from the atmosphere by 2100 using a portfolio of CO 2 removal (CDR) methods. Ocean afforestation, CDR through basin-scale seaweed farming in the ope...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Bach, Lennart T., Tamsitt, Veronica, Gower, Jim, Hurd, Catriona L., Raven, John A., Boyd, Philip W.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2021
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Online Access:http://dx.doi.org/10.1038/s41467-021-22837-2
http://www.nature.com/articles/s41467-021-22837-2.pdf
http://www.nature.com/articles/s41467-021-22837-2
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Summary:Abstract Ensuring that global warming remains <2 °C requires rapid CO 2 emissions reduction. Additionally, 100–900 gigatons CO 2 must be removed from the atmosphere by 2100 using a portfolio of CO 2 removal (CDR) methods. Ocean afforestation, CDR through basin-scale seaweed farming in the open ocean, is seen as a key component of the marine portfolio. Here, we analyse the CDR potential of recent re-occurring trans-basin belts of the floating seaweed Sargassum in the (sub)tropical North Atlantic as a natural analogue for ocean afforestation. We show that two biogeochemical feedbacks, nutrient reallocation and calcification by encrusting marine life, reduce the CDR efficacy of Sargassum by 20–100%. Atmospheric CO 2 influx into the surface seawater, after CO 2 -fixation by Sargassum , takes 2.5–18 times longer than the CO 2 -deficient seawater remains in contact with the atmosphere, potentially hindering CDR verification. Furthermore, we estimate that increased ocean albedo, due to floating Sargassum , could influence climate radiative forcing more than Sargassum -CDR. Our analysis shows that multifaceted Earth-system feedbacks determine the efficacy of ocean afforestation.