The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model

Abstract We investigate the relative importance of ecosystem complexity and phytoplankton light absorption for climate studies. While the complexity of Earth System models (ESMs) with respect to marine biota has increased over the past years, the relative importance of biological processes in drivin...

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Autores principales: Rémy Asselot, Frank Lunkeit, Philip B. Holden, Inga Hense
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Publicado: American Geophysical Union (AGU) 2021
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Acceso en línea:https://doaj.org/article/0a7555ea2679418aa46fadf03dee34b0
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spelling oai:doaj.org-article:0a7555ea2679418aa46fadf03dee34b02021-11-24T08:11:41ZThe Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model1942-246610.1029/2020MS002110https://doaj.org/article/0a7555ea2679418aa46fadf03dee34b02021-05-01T00:00:00Zhttps://doi.org/10.1029/2020MS002110https://doaj.org/toc/1942-2466Abstract We investigate the relative importance of ecosystem complexity and phytoplankton light absorption for climate studies. While the complexity of Earth System models (ESMs) with respect to marine biota has increased over the past years, the relative importance of biological processes in driving climate‐relevant mechanisms such as the biological carbon pump and phytoplankton light absorption is still unknown. The climate effects of these mechanisms have been studied separately, but not together. To shed light on the role of biologically mediated feedbacks, we performed different model experiments with the EcoGENIE ESM. The model experiments have been conducted with and without phytoplankton light absorption and with two or 12 plankton functional types. For a robust comparison, all simulations are tuned to have the same primary production. Our model experiments show that phytoplankton light absorption changes ocean physics and biogeochemistry. Higher sea surface temperature decreases the solubility of CO2 which in turn increases the atmospheric CO2 concentration, and finally the atmospheric temperature rises by 0.45°C. An increase in ecosystem complexity increases the export production of particulate organic carbon but decreases the amount of dissolved organic matter. These changes in the marine carbon cycling, however, hardly reduces the atmospheric CO2 concentrations and slightly decreases the atmospheric temperature by 0.034°C. Overall we show that phytoplankton light absorption has a higher impact on the carbon cycle and on the climate system than a more detailed representation of the marine biota.Rémy AsselotFrank LunkeitPhilip B. HoldenInga HenseAmerican Geophysical Union (AGU)articlecGENIE frameworkEarth system modelecosystem complexityfeedbacklight absorptionmarine ecosystem modelPhysical geographyGB3-5030OceanographyGC1-1581ENJournal of Advances in Modeling Earth Systems, Vol 13, Iss 5, Pp n/a-n/a (2021)
institution DOAJ
collection DOAJ
language EN
topic cGENIE framework
Earth system model
ecosystem complexity
feedback
light absorption
marine ecosystem model
Physical geography
GB3-5030
Oceanography
GC1-1581
spellingShingle cGENIE framework
Earth system model
ecosystem complexity
feedback
light absorption
marine ecosystem model
Physical geography
GB3-5030
Oceanography
GC1-1581
Rémy Asselot
Frank Lunkeit
Philip B. Holden
Inga Hense
The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model
description Abstract We investigate the relative importance of ecosystem complexity and phytoplankton light absorption for climate studies. While the complexity of Earth System models (ESMs) with respect to marine biota has increased over the past years, the relative importance of biological processes in driving climate‐relevant mechanisms such as the biological carbon pump and phytoplankton light absorption is still unknown. The climate effects of these mechanisms have been studied separately, but not together. To shed light on the role of biologically mediated feedbacks, we performed different model experiments with the EcoGENIE ESM. The model experiments have been conducted with and without phytoplankton light absorption and with two or 12 plankton functional types. For a robust comparison, all simulations are tuned to have the same primary production. Our model experiments show that phytoplankton light absorption changes ocean physics and biogeochemistry. Higher sea surface temperature decreases the solubility of CO2 which in turn increases the atmospheric CO2 concentration, and finally the atmospheric temperature rises by 0.45°C. An increase in ecosystem complexity increases the export production of particulate organic carbon but decreases the amount of dissolved organic matter. These changes in the marine carbon cycling, however, hardly reduces the atmospheric CO2 concentrations and slightly decreases the atmospheric temperature by 0.034°C. Overall we show that phytoplankton light absorption has a higher impact on the carbon cycle and on the climate system than a more detailed representation of the marine biota.
format article
author Rémy Asselot
Frank Lunkeit
Philip B. Holden
Inga Hense
author_facet Rémy Asselot
Frank Lunkeit
Philip B. Holden
Inga Hense
author_sort Rémy Asselot
title The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model
title_short The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model
title_full The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model
title_fullStr The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model
title_full_unstemmed The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model
title_sort relative importance of phytoplankton light absorption and ecosystem complexity in an earth system model
publisher American Geophysical Union (AGU)
publishDate 2021
url https://doaj.org/article/0a7555ea2679418aa46fadf03dee34b0
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