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...
Published in: | Biogeosciences |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
2021
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Subjects: | |
Online Access: | https://doi.org/10.5194/bg-18-4389-2021 https://bg.copernicus.org/articles/18/4389/2021/ |