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    Interactive comment on “The Plio-Pleistocene climatic evolution as a consequence of orbital forcing on the carbon cycle” by Didier Paillard (2017)
    COPERNICUS GESELLSCHAFT MBH
    In:  EPIC3Climate of the Past Discussions, COPERNICUS GESELLSCHAFT MBH, ISSN: 1814-9324
    Details
    Publication Date: 2017-03-27
    Description: The paper of Paillard investigates the Plio-Pleistocene carbon cycle by setting up a conceptual model, consisting of differential equation for the carbon content of the atmosphere-ocean-biosphere C, the alkalinity of the ocean, A, and the stable carbon isotope values of C, d13C. I find the conceptual idea how to understand the observed long-term changes in the carbon cycle very interesting. However, I have some fundamental comments to Equation 3 describing the evolution of the the carbon isotope of the system.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , notRev
    Format: application/pdf
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