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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Special issue
The CSIRO Mk3L climate system model
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Oceanic sediment cores are commonly used to understand past climates. The composition of the sediments changes with the ocean above it. An understanding of oceanographic conditions that existed many thousands of years ago, in some cases many millions of years ago, can therefore be extracted from sediment cores. We simulate two chemical signatures (13C and 15N) of sediment cores in a model. This study assesses the model before it is applied to reinterpret the sedimentary record.
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GMD | Articles | Volume 12, issue 4
GMD | Articles | Volume 12, issue 4
Geosci. Model Dev., 12, 1491–1523, 2019
https://doi.org/10.5194/gmd-12-1491-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: The CSIRO Mk3L climate system model

Geosci. Model Dev., 12, 1491–1523, 2019
https://doi.org/10.5194/gmd-12-1491-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
GMD | Articles | Volume 12, issue 4

Model description paper 16 Apr 2019

Model description paper | 16 Apr 2019

Ocean carbon and nitrogen isotopes in CSIRO Mk3L-COAL version 1.0: a tool for palaeoceanographic research

Pearse J. Buchanan et al.

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Publications Copernicus
Special issue
The CSIRO Mk3L climate system model
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Short summary
Oceanic sediment cores are commonly used to understand past climates. The composition of the sediments changes with the ocean above it. An understanding of oceanographic conditions that existed many thousands of years ago, in some cases many millions of years ago, can therefore be extracted from sediment cores. We simulate two chemical signatures (13C and 15N) of sediment cores in a model. This study assesses the model before it is applied to reinterpret the sedimentary record.
Read more
Citation
Geoscientific Model Development

An interactive open-access journal of the European Geosciences Union

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