More efficient North Atlantic carbon pump during the Last Glacial Maximum

More efficient North Atlantic carbon pump during the Last Glacial Maximum

Atmospheric CO2 is governed by CO2 gains (e.g., via Southern Ocean outgassing) and losses (e.g., via North Atlantic absorption). Using a novel method to estimate air–sea CO2 exchange signals, the authors show that North Atlantic CO2 absorption became more efficient and contributed to lowering atmosp...

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Autores principales: J. Yu, L. Menviel, Z. D. Jin, D. J. R. Thornalley, G. L. Foster, E. J. Rohling, I. N. McCave, J. F. McManus, Y. Dai, H. Ren, F. He, F. Zhang, P. J. Chen, A. P. Roberts
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
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Q
Acceso en línea:https://doaj.org/article/1dc84fb6a526466ba35c0597c50b0ec2
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spelling oai:doaj.org-article:1dc84fb6a526466ba35c0597c50b0ec22021-12-02T16:58:28ZMore efficient North Atlantic carbon pump during the Last Glacial Maximum10.1038/s41467-019-10028-z2041-1723https://doaj.org/article/1dc84fb6a526466ba35c0597c50b0ec22019-05-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-10028-zhttps://doaj.org/toc/2041-1723Atmospheric CO2 is governed by CO2 gains (e.g., via Southern Ocean outgassing) and losses (e.g., via North Atlantic absorption). Using a novel method to estimate air–sea CO2 exchange signals, the authors show that North Atlantic CO2 absorption became more efficient and contributed to lowering atmospheric CO2 during ice ages.J. YuL. MenvielZ. D. JinD. J. R. ThornalleyG. L. FosterE. J. RohlingI. N. McCaveJ. F. McManusY. DaiH. RenF. HeF. ZhangP. J. ChenA. P. RobertsNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-11 (2019)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
J. Yu
L. Menviel
Z. D. Jin
D. J. R. Thornalley
G. L. Foster
E. J. Rohling
I. N. McCave
J. F. McManus
Y. Dai
H. Ren
F. He
F. Zhang
P. J. Chen
A. P. Roberts
More efficient North Atlantic carbon pump during the Last Glacial Maximum
description Atmospheric CO2 is governed by CO2 gains (e.g., via Southern Ocean outgassing) and losses (e.g., via North Atlantic absorption). Using a novel method to estimate air–sea CO2 exchange signals, the authors show that North Atlantic CO2 absorption became more efficient and contributed to lowering atmospheric CO2 during ice ages.
format article
author J. Yu
L. Menviel
Z. D. Jin
D. J. R. Thornalley
G. L. Foster
E. J. Rohling
I. N. McCave
J. F. McManus
Y. Dai
H. Ren
F. He
F. Zhang
P. J. Chen
A. P. Roberts
author_facet J. Yu
L. Menviel
Z. D. Jin
D. J. R. Thornalley
G. L. Foster
E. J. Rohling
I. N. McCave
J. F. McManus
Y. Dai
H. Ren
F. He
F. Zhang
P. J. Chen
A. P. Roberts
author_sort J. Yu
title More efficient North Atlantic carbon pump during the Last Glacial Maximum
title_short More efficient North Atlantic carbon pump during the Last Glacial Maximum
title_full More efficient North Atlantic carbon pump during the Last Glacial Maximum
title_fullStr More efficient North Atlantic carbon pump during the Last Glacial Maximum
title_full_unstemmed More efficient North Atlantic carbon pump during the Last Glacial Maximum
title_sort more efficient north atlantic carbon pump during the last glacial maximum
publisher Nature Portfolio
publishDate 2019
url https://doaj.org/article/1dc84fb6a526466ba35c0597c50b0ec2
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