Incorporating the stable carbon isotope C-13 in the ocean biogeochemical component of the Max Planck Institute Earth System Model

The stable carbon isotopic composition (delta C-13) is an important variable to study the ocean carbon cycle across different timescales. We include a new representation of the stable carbon isotope C-13 into the HAMburg Ocean Carbon Cycle model (HAMOCC), the ocean biogeochemical component of the Ma...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Liu, Bo, Six, Katharina D., Ilyina, Tatiana
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Gesellschaft Mbh 2021
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00755/86725/92176.pdf
https://archimer.ifremer.fr/doc/00755/86725/92177.pdf
https://doi.org/10.5194/bg-18-4389-2021
https://archimer.ifremer.fr/doc/00755/86725/