Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...

The ocean is a major carbon sink and takes up 25%–30% of the anthropogenically emitted CO2. A state-of-the-art method to quantify this sink are global ocean biogeochemistry models (GOBMs), but their simulated CO2 uptake differs between models and is systematically lower than estimates based on stati...

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Main Authors: Terhaar, Jens, Goris, Nadine, Müller, Jens D., DeVries, Tim, Gruber, Nicolas, Hauck, Judith, Perez, Fiz F., Séférian, Roland
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2024
Subjects:
Online Access:https://dx.doi.org/10.48350/194339
https://boris.unibe.ch/194339/
id ftdatacite:10.48350/194339
record_format openpolar
spelling ftdatacite:10.48350/194339 2024-04-28T08:39:34+00:00 Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ... Terhaar, Jens Goris, Nadine Müller, Jens D. DeVries, Tim Gruber, Nicolas Hauck, Judith Perez, Fiz F. Séférian, Roland 2024 https://dx.doi.org/10.48350/194339 https://boris.unibe.ch/194339/ unknown American Geophysical Union https://dx.doi.org/10.1029/2023MS003840 open access Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 http://purl.org/coar/access_right/c_abf2 530 Physics 550 Earth sciences & geology article-journal Text ScholarlyArticle journal article 2024 ftdatacite https://doi.org/10.48350/19433910.1029/2023MS003840 2024-04-02T11:47:40Z The ocean is a major carbon sink and takes up 25%–30% of the anthropogenically emitted CO2. A state-of-the-art method to quantify this sink are global ocean biogeochemistry models (GOBMs), but their simulated CO2 uptake differs between models and is systematically lower than estimates based on statistical methods using surface ocean pCO2 and interior ocean measurements. Here, we provide an in-depth evaluation of ocean carbon sink estimates from 1980 to 2018 from a GOBM ensemble. As sources of inter-model differences and ensemble-mean biases our study identifies (a) the model setup, such as the length of the spin-up, the starting date of the simulation, and carbon fluxes from rivers and into sediments, (b) the simulated ocean circulation, such as Atlantic Meridional Overturning Circulation and Southern Ocean mode and intermediate water formation, and (c) the simulated oceanic buffer capacity. Our analysis suggests that a late starting date and biases in the ocean circulation cause a too low anthropogenic CO2 ... Article in Journal/Newspaper Southern Ocean DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic 530 Physics
550 Earth sciences & geology
spellingShingle 530 Physics
550 Earth sciences & geology
Terhaar, Jens
Goris, Nadine
Müller, Jens D.
DeVries, Tim
Gruber, Nicolas
Hauck, Judith
Perez, Fiz F.
Séférian, Roland
Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...
topic_facet 530 Physics
550 Earth sciences & geology
description The ocean is a major carbon sink and takes up 25%–30% of the anthropogenically emitted CO2. A state-of-the-art method to quantify this sink are global ocean biogeochemistry models (GOBMs), but their simulated CO2 uptake differs between models and is systematically lower than estimates based on statistical methods using surface ocean pCO2 and interior ocean measurements. Here, we provide an in-depth evaluation of ocean carbon sink estimates from 1980 to 2018 from a GOBM ensemble. As sources of inter-model differences and ensemble-mean biases our study identifies (a) the model setup, such as the length of the spin-up, the starting date of the simulation, and carbon fluxes from rivers and into sediments, (b) the simulated ocean circulation, such as Atlantic Meridional Overturning Circulation and Southern Ocean mode and intermediate water formation, and (c) the simulated oceanic buffer capacity. Our analysis suggests that a late starting date and biases in the ocean circulation cause a too low anthropogenic CO2 ...
format Article in Journal/Newspaper
author Terhaar, Jens
Goris, Nadine
Müller, Jens D.
DeVries, Tim
Gruber, Nicolas
Hauck, Judith
Perez, Fiz F.
Séférian, Roland
author_facet Terhaar, Jens
Goris, Nadine
Müller, Jens D.
DeVries, Tim
Gruber, Nicolas
Hauck, Judith
Perez, Fiz F.
Séférian, Roland
author_sort Terhaar, Jens
title Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...
title_short Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...
title_full Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...
title_fullStr Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...
title_full_unstemmed Assessment of Global Ocean Biogeochemistry Models for Ocean Carbon Sink Estimates in RECCAP2 and Recommendations for Future Studies ...
title_sort assessment of global ocean biogeochemistry models for ocean carbon sink estimates in reccap2 and recommendations for future studies ...
publisher American Geophysical Union
publishDate 2024
url https://dx.doi.org/10.48350/194339
https://boris.unibe.ch/194339/
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://dx.doi.org/10.1029/2023MS003840
op_rights open access
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.48350/19433910.1029/2023MS003840
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