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Future changes in δ13C of dissolved inorganic carbon in the ocean

Abstract:

Emissions of carbon dioxide from fossil fuel combustion are reducing the ratio 13C/12C, δ13C, in atmospheric CO2 and in the carbon in the ocean and terrestrial biosphere that exchanges with the atmosphere on timescales of decades to centuries. Future changes to fossil fuel emissions vary across different scenarios and may cause decreases of more than 6‰ in atmospheric δ13CO2 between 1850 and 2100. The effects of these potential changes on the three-dimensional distribution of δ13C in the ocea...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2021EF002173

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Oxford college:
Linacre College
Role:
Author
Publisher:
Wiley Open Access Publisher's website
Journal:
Earth's Future Journal website
Volume:
9
Issue:
12
Article number:
e2021EF002173
Publication date:
2021-10-01
Acceptance date:
2021-09-26
DOI:
ISSN:
2328-4277
Language:
English
Keywords:
Pubs id:
1198477
Local pid:
pubs:1198477
Deposit date:
2021-10-04

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