Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ
. About 30% has been taken up by the oceans Skeletons and shells of marine calcifiers are made of different crystalline forms of calcium carbonate, such as calcite or aragonite. A decrease in the saturation state of calcium carbonate can result in decreased calcification and increased dissolution of...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1053.7553 2023-05-15T17:51:14+02:00 Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ Published Online The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1053.7553 http://shadow.eas.gatech.edu/%7Ekcobb/ocean_acid/Friedrich%20et%20al%202012.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1053.7553 http://shadow.eas.gatech.edu/%7Ekcobb/ocean_acid/Friedrich%20et%20al%202012.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://shadow.eas.gatech.edu/%7Ekcobb/ocean_acid/Friedrich%20et%20al%202012.pdf text ftciteseerx 2020-04-12T00:18:45Z . About 30% has been taken up by the oceans Skeletons and shells of marine calcifiers are made of different crystalline forms of calcium carbonate, such as calcite or aragonite. A decrease in the saturation state of calcium carbonate can result in decreased calcification and increased dissolution of calcium carbonate Here we present results from a model simulation over 1,300 years (800-2099 ad) that was conducted with a state-of-the-art coupled carbon cycle-climate model (MPI-ESM, see Supplementary Information for details) forced by the most recent reconstructions of solar and volcanic radiative perturbations, land-use changes, aerosols and orbital variations. The model is also subject to historical CO 2 emissions and the A1B greenhouse-gas emission scenario ( According to the MPI-ESM simulation of the pre-industrial surface waters, local marine ecosystems have been exposed to a diverse range of natural variability in both the amplitude of the annual cycle and the interannual variability of Ω surf Ar ( Text Ocean acidification Unknown |
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. About 30% has been taken up by the oceans Skeletons and shells of marine calcifiers are made of different crystalline forms of calcium carbonate, such as calcite or aragonite. A decrease in the saturation state of calcium carbonate can result in decreased calcification and increased dissolution of calcium carbonate Here we present results from a model simulation over 1,300 years (800-2099 ad) that was conducted with a state-of-the-art coupled carbon cycle-climate model (MPI-ESM, see Supplementary Information for details) forced by the most recent reconstructions of solar and volcanic radiative perturbations, land-use changes, aerosols and orbital variations. The model is also subject to historical CO 2 emissions and the A1B greenhouse-gas emission scenario ( According to the MPI-ESM simulation of the pre-industrial surface waters, local marine ecosystems have been exposed to a diverse range of natural variability in both the amplitude of the annual cycle and the interannual variability of Ω surf Ar ( |
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Published Online Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
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Published Online |
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title |
Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
title_short |
Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
title_full |
Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
title_fullStr |
Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
title_full_unstemmed |
Detecting regional anthropogenic trends in ocean acidification against natural variability Since the beginning of the Industrial Revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
title_sort |
detecting regional anthropogenic trends in ocean acidification against natural variability since the beginning of the industrial revolution humans have released ∼500 billion metric tons of carbon to the atmosphere through fossil-fuel burning, cement produ |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1053.7553 http://shadow.eas.gatech.edu/%7Ekcobb/ocean_acid/Friedrich%20et%20al%202012.pdf |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
http://shadow.eas.gatech.edu/%7Ekcobb/ocean_acid/Friedrich%20et%20al%202012.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1053.7553 http://shadow.eas.gatech.edu/%7Ekcobb/ocean_acid/Friedrich%20et%20al%202012.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766158325794209792 |