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...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications (EGU)
2021
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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 |