Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2

The increase of atmospheric CO2 (ref. 1) has been predicted to impact the seasonal cycle of inorganic carbon in the global ocean2,3, yet the observational evidence to verify this prediction has been missing. Here, using an observation-based product of the oceanic partial pressure of CO2 (pCO2) cover...

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Published in:Nature Climate Change
Main Authors: Landschützer, Peter, Gruber, Nicolas, Bakker, Dorothee C. E., Stemmler, Irene, Six, Katharina D.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/66135/
https://ueaeprints.uea.ac.uk/id/eprint/66135/1/Figure_4.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/2/Supplementary_information.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/3/Accepted_manuscript.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/4/Figure_1.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/5/Figure_2.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/6/Figure_3.pdf
https://doi.org/10.1038/s41558-017-0057-x
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spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:66135 2023-05-15T17:51:21+02:00 Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2 Landschützer, Peter Gruber, Nicolas Bakker, Dorothee C. E. Stemmler, Irene Six, Katharina D. 2018-01-29 application/pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/ https://ueaeprints.uea.ac.uk/id/eprint/66135/1/Figure_4.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/2/Supplementary_information.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/3/Accepted_manuscript.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/4/Figure_1.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/5/Figure_2.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/6/Figure_3.pdf https://doi.org/10.1038/s41558-017-0057-x en eng https://ueaeprints.uea.ac.uk/id/eprint/66135/1/Figure_4.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/2/Supplementary_information.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/3/Accepted_manuscript.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/4/Figure_1.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/5/Figure_2.pdf https://ueaeprints.uea.ac.uk/id/eprint/66135/6/Figure_3.pdf Landschützer, Peter, Gruber, Nicolas, Bakker, Dorothee C. E., Stemmler, Irene and Six, Katharina D. (2018) Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2. Nature Climate Change, 8. 146–150. ISSN 1758-678X doi:10.1038/s41558-017-0057-x Article PeerReviewed 2018 ftuniveastangl https://doi.org/10.1038/s41558-017-0057-x 2023-03-23T23:32:23Z The increase of atmospheric CO2 (ref. 1) has been predicted to impact the seasonal cycle of inorganic carbon in the global ocean2,3, yet the observational evidence to verify this prediction has been missing. Here, using an observation-based product of the oceanic partial pressure of CO2 (pCO2) covering the past 34 years, we find that the winter-to-summer difference of the pCO2 has increased on average by 2.2 ± 0.4 μatm per decade from 1982 to 2015 poleward of 10° latitude. This is largely in agreement with the trend expected from thermodynamic considerations. Most of the increase stems from the seasonality of the drivers acting on an increasing oceanic pCO2 caused by the uptake of anthropogenic CO2 from the atmosphere. In the high latitudes, the concurrent ocean-acidification-induced changes in the buffer capacity of the ocean enhance this effect. This strengthening of the seasonal winter-to-summer difference pushes the global ocean towards critical thresholds earlier, inducing stress to ocean ecosystems and fisheries4. Our study provides observational evidence for this strengthening seasonal difference in the oceanic carbon cycle on a global scale, illustrating the inevitable consequences of anthropogenic CO2 emissions. Article in Journal/Newspaper Ocean acidification University of East Anglia: UEA Digital Repository Nature Climate Change 8 2 146 150
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collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language English
description The increase of atmospheric CO2 (ref. 1) has been predicted to impact the seasonal cycle of inorganic carbon in the global ocean2,3, yet the observational evidence to verify this prediction has been missing. Here, using an observation-based product of the oceanic partial pressure of CO2 (pCO2) covering the past 34 years, we find that the winter-to-summer difference of the pCO2 has increased on average by 2.2 ± 0.4 μatm per decade from 1982 to 2015 poleward of 10° latitude. This is largely in agreement with the trend expected from thermodynamic considerations. Most of the increase stems from the seasonality of the drivers acting on an increasing oceanic pCO2 caused by the uptake of anthropogenic CO2 from the atmosphere. In the high latitudes, the concurrent ocean-acidification-induced changes in the buffer capacity of the ocean enhance this effect. This strengthening of the seasonal winter-to-summer difference pushes the global ocean towards critical thresholds earlier, inducing stress to ocean ecosystems and fisheries4. Our study provides observational evidence for this strengthening seasonal difference in the oceanic carbon cycle on a global scale, illustrating the inevitable consequences of anthropogenic CO2 emissions.
format Article in Journal/Newspaper
author Landschützer, Peter
Gruber, Nicolas
Bakker, Dorothee C. E.
Stemmler, Irene
Six, Katharina D.
spellingShingle Landschützer, Peter
Gruber, Nicolas
Bakker, Dorothee C. E.
Stemmler, Irene
Six, Katharina D.
Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2
author_facet Landschützer, Peter
Gruber, Nicolas
Bakker, Dorothee C. E.
Stemmler, Irene
Six, Katharina D.
author_sort Landschützer, Peter
title Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2
title_short Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2
title_full Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2
title_fullStr Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2
title_full_unstemmed Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2
title_sort strengthening seasonal marine co2 variations due to increasing atmospheric co2
publishDate 2018
url https://ueaeprints.uea.ac.uk/id/eprint/66135/
https://ueaeprints.uea.ac.uk/id/eprint/66135/1/Figure_4.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/2/Supplementary_information.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/3/Accepted_manuscript.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/4/Figure_1.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/5/Figure_2.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/6/Figure_3.pdf
https://doi.org/10.1038/s41558-017-0057-x
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://ueaeprints.uea.ac.uk/id/eprint/66135/1/Figure_4.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/2/Supplementary_information.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/3/Accepted_manuscript.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/4/Figure_1.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/5/Figure_2.pdf
https://ueaeprints.uea.ac.uk/id/eprint/66135/6/Figure_3.pdf
Landschützer, Peter, Gruber, Nicolas, Bakker, Dorothee C. E., Stemmler, Irene and Six, Katharina D. (2018) Strengthening seasonal marine CO2 variations due to increasing atmospheric CO2. Nature Climate Change, 8. 146–150. ISSN 1758-678X
doi:10.1038/s41558-017-0057-x
op_doi https://doi.org/10.1038/s41558-017-0057-x
container_title Nature Climate Change
container_volume 8
container_issue 2
container_start_page 146
op_container_end_page 150
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