EGU2020-5207
https://doi.org/10.5194/egusphere-egu2020-5207
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ocean-atmosphere fluxes of carbon dioxide and heat in response to phytoplankton light absorption

Rémy Asselot1, Frank Lunkeit2, Phil Holden3, and Inga Hense1
Rémy Asselot et al.
  • 1Institute of Hydrobiology and Fisheries Science, Center for Earth System Research and Sustainability, University of Hamburg, Hamburg, Germany
  • 2Meteorological Institute, University of Hamburg, Hamburg, Germany
  • 3Environment, Earth and Ecosystems, The Open University, Walton Hall, Milton Keynes, MK7 6AA, United Kingdom

Oceanic phytoplankton absorbing solar radiation can influence the upper ocean physics. This process is called phytoplankton light absorption. Previous studies indicate that phytoplankton light absorption significantly impacts the oceanic heat distribution and, if taken into account in an Earth System model, can lead to different climates under similar primary production. However, the dominant processes responsible for these drastic changes in atmospheric temperature have not been yet identified. Phytoplankton light absorption increases the sea surface temperature, therefore altering the exchange of heat between the ocean and the atmosphere. Additionally, phytoplankton light absorption indirectly modifies the ocean carbon cycle and thus the CO2 flux into the atmosphere. To shed light on these aspects, we use an Earth System model of intermediate complexity coupled to an ecosystem model (EcoGENIE). By running a suite of experiements, we determine which fluxes are most important in controlling atmospheric temperature. Here, we present first results of our study.

How to cite: Asselot, R., Lunkeit, F., Holden, P., and Hense, I.: Ocean-atmosphere fluxes of carbon dioxide and heat in response to phytoplankton light absorption, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5207, https://doi.org/10.5194/egusphere-egu2020-5207, 2020.