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

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

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Liu, Bo, Six, Katharina D., Ilyina, Tatiana
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/bg-18-4389-2021
https://bg.copernicus.org/articles/18/4389/2021/