hdl:10013/epic.50629
Interactive comment on “The Plio-Pleistocene climatic evolution as a consequence of orbital forcing on the carbon cycle” by Didier Paillard
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Peter.Koehler [ at ] awi.de
Abstract
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.
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Article
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Primary Division
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Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Publication Status
Published
Eprint ID
44288
DOI
10.5194/cp-2017-3-SC1
![[thumbnail of koehler2017cpd.pdf]](https://epic.awi.de/44288/1.hassmallThumbnailVersion/koehler2017cpd.pdf)
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Köhler, P.
(2017):
Interactive comment on “The Plio-Pleistocene climatic evolution as a consequence of orbital forcing on the carbon cycle” by Didier Paillard
,
Climate of the Past Discussions
.
doi: 10.5194/cp-2017-3-SC1
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