Home Database Research and knowledge projects Origin and fate of biogenic particle fluxes in the ocean and their interaction with the atmospheric CO2 concentration as well as the marine sediment.
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Project

Origin and fate of biogenic particle fluxes in the ocean and their interaction with the atmospheric CO2 concentration as well as the marine sediment. (ORFOIS)

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Description:

The main scientific objectives of project ORFOIS are to:

  • identify and quantify globally the mechanisms underlying the transformation of biogenic particles to dissolved substances within the ocean water column in order to predict correctly surface ocean carbon dioxide sources and sinks;
  • develop a refined particle flux model for operational use in ocean general circulation models which realistically describes particle dynamics in the water column, deposition of material to the sediment, and the interaction with the carbon dioxide partial pressure pCO2;
  • provide a global closed carbon and nutrient budget for modern (preindustrial) conditions including the water column sediment interaction;
  • estimate the changes in CO2 sea surface source sink patterns and vertical redistributions of carbon as well as nutrients for future global change, climate change as well as carbon sequestration scenarios including the associated potential economic impacts.

The ORFOIS project focused on the origin and fate of biogenic particle fluxes in the ocean and their interaction with the atmospheric CO2, as well as the marine sediment. Part of the project objectives included the development of a refined particle flux model for operational use in ocean general circulation models. The improved model needs to realistically describe particle dynamics in the water column, deposition of material to the sediment and the interaction with the partial pressure of CO2 (pCO2).

Compared to other state-of-the-art closed system models (Hamburg Model of the Ocean Carbon Cycle) the newly improved model is more realistic and more sensitive to changes in the potential driving mechanisms for glacial pCO2 reduction.

Project information

Lead

UNIVERSITY OF WESTERN BRITTANY Nicolas Dittert

Partners

University of Bergen; Danmarks Miljøundersøgelser National Environmental Research Institute; Laboratoire des Sciences du Climat et de l'Environnement; Institut Universitaire Européen de la Mer; Max-Planck-Institut für Meteorologie; Institute for Marine Environmental Sciences Universität Bremen; Forschungsstelle Nachhaltige Umweltentwicklung Zentrum für Meeres- und Klimaforschung Universität Hamburg; Institute of Oceanography Hellenic Center for Marine Research; Centre for Estuarine and Coastal Ecology Netherlands Institute of Ecology; School of Environmental Sciences University of East Anglia

Source of funding

FP 5

Published in Climate-ADAPT Jun 07 2016   -   Last Modified in Climate-ADAPT Dec 12 2023

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