Articles | Volume 15, issue 4
https://doi.org/10.5194/esd-15-875-2024
https://doi.org/10.5194/esd-15-875-2024
Research article
 | 
15 Jul 2024
Research article |  | 15 Jul 2024

A missing link in the carbon cycle: phytoplankton light absorption under RCP emission scenarios

Rémy Asselot, Philip B. Holden, Frank Lunkeit, and Inga Hense

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Climate pathways behind phytoplankton-induced atmospheric warming
Rémy Asselot, Frank Lunkeit, Philip B. Holden, and Inga Hense
Biogeosciences, 19, 223–239, https://doi.org/10.5194/bg-19-223-2022,https://doi.org/10.5194/bg-19-223-2022, 2022
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A missing link in the carbon cycle: phytoplankton light absorption
Rémy Asselot, Frank Lunkeit, Philip Holden, and Inga Hense
Earth Syst. Dynam. Discuss., https://doi.org/10.5194/esd-2021-91,https://doi.org/10.5194/esd-2021-91, 2021
Revised manuscript not accepted
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Cited articles

Anderson, S., Barton, A., Clayton, S., Dutkiewicz, S., and Rynearson, T.: Marine phytoplankton functional types exhibit diverse responses to thermal change, Nat. Commun., 12, 1–9, 2021. a
Anderson, W., Gnanadesikan, A., Hallberg, R., Dunne, J., and Samuels, B.: Impact of ocean color on the maintenance of the Pacific Cold Tongue, Geophys. Res. Lett., 34, L11609, https://doi.org/10.1029/2007GL030100, 2007. a
Asselot, R., Lunkeit, F., Holden, P. B., and Hense, I.: The relative importance of phytoplankton light absorption and ecosystem complexity in an Earth system model, J. Adv. Model. Earth Sy., 13, e2020MS002110, https://doi.org/10.1029/2020MS002110, 2021. a, b, c, d, e, f, g, h, i, j, k, l, m, n, o, p, q, r, s, t
Asselot, R., Lunkeit, F., Holden, P. B., and Hense, I.: Climate pathways behind phytoplankton-induced atmospheric warming, Biogeosciences, 19, 223–239, https://doi.org/10.5194/bg-19-223-2022, 2022. a, b, c, d, e
Behrenfeld, M. J. and Falkowski, P. G.: Photosynthetic rates derived from satellite–based chlorophyll concentration, Limnol. Oceanogr., 42, 1–20, 1997. a
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Phytoplankton are tiny oceanic algae able to absorb the light penetrating the ocean. The light absorbed by these organisms is re-emitted as heat in the surrounding environment, a process commonly called phytoplankton light absorption (PLA). As a consequence, PLA increases the oceanic temperature. We studied this mechanism with a climate model under different climate scenarios. We show that phytoplankton light absorption is reduced under strong warming scenarios, limiting oceanic warming.
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