www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License.
Abstract. At present, although seasonal sea-ice cover mit-igates atmosphere-ocean gas exchange, the Arctic Ocean takes up carbon dioxide (CO2) on the order of −66 to −199 Tg C year−1 (1012 g C), contributing 5–14 % to the global balance of CO2 sinks and sources. Because of this, the Arctic Ocean has...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.504.5497 2023-05-15T14:36:56+02:00 www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. N. R. Bates J. T. Mathis The Pennsylvania State University CiteSeerX Archives 2009 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.5497 http://www.biogeosciences.net/6/2433/2009/bg-6-2433-2009.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.5497 http://www.biogeosciences.net/6/2433/2009/bg-6-2433-2009.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.biogeosciences.net/6/2433/2009/bg-6-2433-2009.pdf text 2009 ftciteseerx 2016-01-08T09:18:27Z Abstract. At present, although seasonal sea-ice cover mit-igates atmosphere-ocean gas exchange, the Arctic Ocean takes up carbon dioxide (CO2) on the order of −66 to −199 Tg C year−1 (1012 g C), contributing 5–14 % to the global balance of CO2 sinks and sources. Because of this, the Arctic Ocean has an important influence on the global carbon cycle, with the marine carbon cycle and atmosphere-ocean CO2 exchanges sensitive to Arctic Ocean and global climate change feedbacks. In the near-term, further sea-ice loss and increases in phytoplankton growth rates are expected to in-crease the uptake of CO2 by Arctic Ocean surface waters, al-though mitigated somewhat by surface warming in the Arc-tic. Thus, the capacity of the Arctic Ocean to uptake CO2 is expected to alter in response to environmental changes driven largely by climate. These changes are likely to con-tinue to modify the physics, biogeochemistry, and ecology of the Arctic Ocean in ways that are not yet fully understood. In surface waters, sea-ice melt, river runoff, cooling and uptake of CO2 through air-sea gas exchange combine to decrease the calcium carbonate (CaCO3) mineral saturation states () of seawater while seasonal phytoplankton primary production (PP) mitigates this effect. Biological amplification of ocean acidification effects in subsurface waters, due to the reminer-alization of organic matter, is likely to reduce the ability of many species to produce CaCO3 shells or tests with profound implications for Arctic marine ecosystems 1 Text Arctic Arctic Ocean Climate change Ocean acidification Phytoplankton Sea ice Unknown Arctic Arctic Ocean |
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Unknown |
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ftciteseerx |
language |
English |
description |
Abstract. At present, although seasonal sea-ice cover mit-igates atmosphere-ocean gas exchange, the Arctic Ocean takes up carbon dioxide (CO2) on the order of −66 to −199 Tg C year−1 (1012 g C), contributing 5–14 % to the global balance of CO2 sinks and sources. Because of this, the Arctic Ocean has an important influence on the global carbon cycle, with the marine carbon cycle and atmosphere-ocean CO2 exchanges sensitive to Arctic Ocean and global climate change feedbacks. In the near-term, further sea-ice loss and increases in phytoplankton growth rates are expected to in-crease the uptake of CO2 by Arctic Ocean surface waters, al-though mitigated somewhat by surface warming in the Arc-tic. Thus, the capacity of the Arctic Ocean to uptake CO2 is expected to alter in response to environmental changes driven largely by climate. These changes are likely to con-tinue to modify the physics, biogeochemistry, and ecology of the Arctic Ocean in ways that are not yet fully understood. In surface waters, sea-ice melt, river runoff, cooling and uptake of CO2 through air-sea gas exchange combine to decrease the calcium carbonate (CaCO3) mineral saturation states () of seawater while seasonal phytoplankton primary production (PP) mitigates this effect. Biological amplification of ocean acidification effects in subsurface waters, due to the reminer-alization of organic matter, is likely to reduce the ability of many species to produce CaCO3 shells or tests with profound implications for Arctic marine ecosystems 1 |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
N. R. Bates J. T. Mathis |
spellingShingle |
N. R. Bates J. T. Mathis www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. |
author_facet |
N. R. Bates J. T. Mathis |
author_sort |
N. R. Bates |
title |
www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_short |
www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_full |
www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_fullStr |
www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_full_unstemmed |
www.biogeosciences.net/6/2433/2009/ © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_sort |
www.biogeosciences.net/6/2433/2009/ © author(s) 2009. this work is distributed under the creative commons attribution 3.0 license. |
publishDate |
2009 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.5497 http://www.biogeosciences.net/6/2433/2009/bg-6-2433-2009.pdf |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Climate change Ocean acidification Phytoplankton Sea ice |
genre_facet |
Arctic Arctic Ocean Climate change Ocean acidification Phytoplankton Sea ice |
op_source |
http://www.biogeosciences.net/6/2433/2009/bg-6-2433-2009.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.504.5497 http://www.biogeosciences.net/6/2433/2009/bg-6-2433-2009.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766309457011146752 |