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

Direct comparison between paleo oceanic δ13C records and model results facilitates assessing simulated distributions and properties of water masses in the past. To accomplish this, we include a new representation of the stable carbon isotope 13C into the HAMburg Ocean Carbon Cycle model (HAMOCC), th...

Full description

Bibliographic Details
Main Authors: Liu, Bo, Six, Katharina D., Ilyina, Tatiana
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications (EGU) 2021
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/52513/
https://oceanrep.geomar.de/id/eprint/52513/1/bg-2021-32.pdf
https://doi.org/10.5194/bg-2021-32