The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble
The oceans currently take up around a quarter of the carbon dioxide (CO<sub>2</sub>) emitted by human activity. While stored in the ocean, this CO<sub>2</sub> is not influencing Earth's radiation budget; the ocean CO<sub>2</sub> sink therefore plays an import...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2015-07-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/12/4497/2015/bg-12-4497-2015.pdf |
| _version_ | 1818513179601272832 |
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| author | P. R. Halloran B. B. B. Booth C. D. Jones F. H. Lambert D. J. McNeall I. J. Totterdell C. Völker |
| author_facet | P. R. Halloran B. B. B. Booth C. D. Jones F. H. Lambert D. J. McNeall I. J. Totterdell C. Völker |
| author_sort | P. R. Halloran |
| collection | DOAJ |
| description | The oceans currently take up around a quarter of the carbon dioxide (CO<sub>2</sub>)
emitted by human activity. While stored in the ocean, this CO<sub>2</sub> is not
influencing Earth's radiation budget; the ocean CO<sub>2</sub> sink therefore plays
an important role in mitigating global warming. CO<sub>2</sub> uptake by the oceans
is heterogeneous, with the subpolar North Atlantic being the strongest CO<sub>2</sub>
sink region. Observations over the last 2 decades have indicated that
CO<sub>2</sub> uptake by the subpolar North Atlantic sink can vary rapidly. Given the
importance of this sink and its apparent variability, it is critical that we
understand the mechanisms behind its operation. Here we explore the combined
natural and anthropogenic subpolar North Atlantic CO<sub>2</sub> uptake across a
large ensemble of Earth System Model simulations, and find that models show a
peak in sink strength around the middle of the century after which CO<sub>2</sub>
uptake begins to decline. We identify different drivers of change on
interannual and multidecadal timescales. Short-term variability appears to be
driven by fluctuations in regional seawater temperature and alkalinity,
whereas the longer-term evolution throughout the coming century is largely
occurring through a counterintuitive response to rising atmospheric CO<sub>2</sub>
concentrations. At high atmospheric CO<sub>2</sub> concentrations the contrasting
Revelle factors between the low latitude water and the subpolar gyre,
combined with the transport of surface waters from the low latitudes to the
subpolar gyre, means that the subpolar CO<sub>2</sub> uptake capacity is largely
satisfied from its southern boundary rather than through air–sea CO<sub>2</sub> flux.
Our findings indicate that: (i) we can explain the mechanisms of subpolar
North Atlantic CO<sub>2</sub> uptake variability across a broad range of Earth System
Models; (ii) a focus on understanding the mechanisms behind contemporary
variability may not directly tell us about how the sink will change in the
future; (iii) to identify long-term change in the North Atlantic CO<sub>2</sub> sink
we should focus observational resources on monitoring lower latitude as well
as the subpolar seawater CO<sub>2</sub>; (iv) recent observations of a weakening
subpolar North Atlantic CO<sub>2</sub> sink may suggest that the sink strength has
peaked and is in long-term decline. |
| first_indexed | 2024-12-10T23:57:35Z |
| format | Article |
| id | doaj.art-eea3893cfd9d4d218d197af066c13aa1 |
| institution | Directory Open Access Journal |
| issn | 1726-4170 1726-4189 |
| language | English |
| last_indexed | 2024-12-10T23:57:35Z |
| publishDate | 2015-07-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Biogeosciences |
| spelling | doaj.art-eea3893cfd9d4d218d197af066c13aa12022-12-22T01:28:34ZengCopernicus PublicationsBiogeosciences1726-41701726-41892015-07-0112144497450810.5194/bg-12-4497-2015The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensembleP. R. Halloran0B. B. B. Booth1C. D. Jones2F. H. Lambert3D. J. McNeall4I. J. Totterdell5C. Völker6Geography, College of Life and Environmental Sciences, University of Exeter, Amory Building, Rennes Drive, Exeter, EX4 4RJ, UKMet Office Hadley Centre, FitzRoy Road, Exeter, Devon, EX1 3PB, UKMet Office Hadley Centre, FitzRoy Road, Exeter, Devon, EX1 3PB, UKExeter Climate Systems, College of Engineering, Mathematics and Physical Sciences, University of Exeter, Harrison Building, North Park Road, Exeter, EX4 4QF, UKMet Office Hadley Centre, FitzRoy Road, Exeter, Devon, EX1 3PB, UKMet Office Hadley Centre, FitzRoy Road, Exeter, Devon, EX1 3PB, UKAlfred Wegener Institute Helmholz Center for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, GermanyThe oceans currently take up around a quarter of the carbon dioxide (CO<sub>2</sub>) emitted by human activity. While stored in the ocean, this CO<sub>2</sub> is not influencing Earth's radiation budget; the ocean CO<sub>2</sub> sink therefore plays an important role in mitigating global warming. CO<sub>2</sub> uptake by the oceans is heterogeneous, with the subpolar North Atlantic being the strongest CO<sub>2</sub> sink region. Observations over the last 2 decades have indicated that CO<sub>2</sub> uptake by the subpolar North Atlantic sink can vary rapidly. Given the importance of this sink and its apparent variability, it is critical that we understand the mechanisms behind its operation. Here we explore the combined natural and anthropogenic subpolar North Atlantic CO<sub>2</sub> uptake across a large ensemble of Earth System Model simulations, and find that models show a peak in sink strength around the middle of the century after which CO<sub>2</sub> uptake begins to decline. We identify different drivers of change on interannual and multidecadal timescales. Short-term variability appears to be driven by fluctuations in regional seawater temperature and alkalinity, whereas the longer-term evolution throughout the coming century is largely occurring through a counterintuitive response to rising atmospheric CO<sub>2</sub> concentrations. At high atmospheric CO<sub>2</sub> concentrations the contrasting Revelle factors between the low latitude water and the subpolar gyre, combined with the transport of surface waters from the low latitudes to the subpolar gyre, means that the subpolar CO<sub>2</sub> uptake capacity is largely satisfied from its southern boundary rather than through air–sea CO<sub>2</sub> flux. Our findings indicate that: (i) we can explain the mechanisms of subpolar North Atlantic CO<sub>2</sub> uptake variability across a broad range of Earth System Models; (ii) a focus on understanding the mechanisms behind contemporary variability may not directly tell us about how the sink will change in the future; (iii) to identify long-term change in the North Atlantic CO<sub>2</sub> sink we should focus observational resources on monitoring lower latitude as well as the subpolar seawater CO<sub>2</sub>; (iv) recent observations of a weakening subpolar North Atlantic CO<sub>2</sub> sink may suggest that the sink strength has peaked and is in long-term decline.http://www.biogeosciences.net/12/4497/2015/bg-12-4497-2015.pdf |
| spellingShingle | P. R. Halloran B. B. B. Booth C. D. Jones F. H. Lambert D. J. McNeall I. J. Totterdell C. Völker The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble Biogeosciences |
| title | The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble |
| title_full | The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble |
| title_fullStr | The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble |
| title_full_unstemmed | The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble |
| title_short | The mechanisms of North Atlantic CO<sub>2</sub> uptake in a large Earth System Model ensemble |
| title_sort | mechanisms of north atlantic co sub 2 sub uptake in a large earth system model ensemble |
| url | http://www.biogeosciences.net/12/4497/2015/bg-12-4497-2015.pdf |
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