Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model

Ocean acidification from the uptake of anthropogenic carbon is simulated for the industrial period and IPCC SRES emission scenarios A2 and B1 with a global coupled carbon cycle-climate model. Earlier studies identified seawater saturation state with respect to aragonite, a mineral phase of calcium c...

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Main Authors: M. Steinacher, F. Joos, T. L. Frölicher, G.-K. Plattner, S. C. Doney
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://doaj.org/article/a89ccdb47fce436cb17da2a9fe80b782
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spelling ftdoajarticles:oai:doaj.org/article:a89ccdb47fce436cb17da2a9fe80b782 2023-05-15T14:41:25+02:00 Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model M. Steinacher F. Joos T. L. Frölicher G.-K. Plattner S. C. Doney 2009-04-01T00:00:00Z https://doaj.org/article/a89ccdb47fce436cb17da2a9fe80b782 EN eng Copernicus Publications http://www.biogeosciences.net/6/515/2009/bg-6-515-2009.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 https://doaj.org/article/a89ccdb47fce436cb17da2a9fe80b782 Biogeosciences, Vol 6, Iss 4, Pp 515-533 (2009) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2009 ftdoajarticles 2022-12-30T21:39:11Z Ocean acidification from the uptake of anthropogenic carbon is simulated for the industrial period and IPCC SRES emission scenarios A2 and B1 with a global coupled carbon cycle-climate model. Earlier studies identified seawater saturation state with respect to aragonite, a mineral phase of calcium carbonate, as a key variable governing impacts on corals and other shell-forming organisms. Globally in the A2 scenario, water saturated by more than 300%, considered suitable for coral growth, vanishes by 2070 AD (CO 2 ≈630 ppm), and the ocean volume fraction occupied by saturated water decreases from 42% to 25% over this century. The largest simulated pH changes worldwide occur in Arctic surface waters, where hydrogen ion concentration increases by up to 185% (ΔpH=−0.45). Projected climate change amplifies the decrease in Arctic surface mean saturation and pH by more than 20%, mainly due to freshening and increased carbon uptake in response to sea ice retreat. Modeled saturation compares well with observation-based estimates along an Arctic transect and simulated changes have been corrected for remaining model-data differences in this region. Aragonite undersaturation in Arctic surface waters is projected to occur locally within a decade and to become more widespread as atmospheric CO 2 continues to grow. The results imply that surface waters in the Arctic Ocean will become corrosive to aragonite, with potentially large implications for the marine ecosystem, if anthropogenic carbon emissions are not reduced and atmospheric CO 2 not kept below 450 ppm. Article in Journal/Newspaper Arctic Arctic Ocean Climate change Ocean acidification Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
M. Steinacher
F. Joos
T. L. Frölicher
G.-K. Plattner
S. C. Doney
Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
description Ocean acidification from the uptake of anthropogenic carbon is simulated for the industrial period and IPCC SRES emission scenarios A2 and B1 with a global coupled carbon cycle-climate model. Earlier studies identified seawater saturation state with respect to aragonite, a mineral phase of calcium carbonate, as a key variable governing impacts on corals and other shell-forming organisms. Globally in the A2 scenario, water saturated by more than 300%, considered suitable for coral growth, vanishes by 2070 AD (CO 2 ≈630 ppm), and the ocean volume fraction occupied by saturated water decreases from 42% to 25% over this century. The largest simulated pH changes worldwide occur in Arctic surface waters, where hydrogen ion concentration increases by up to 185% (ΔpH=−0.45). Projected climate change amplifies the decrease in Arctic surface mean saturation and pH by more than 20%, mainly due to freshening and increased carbon uptake in response to sea ice retreat. Modeled saturation compares well with observation-based estimates along an Arctic transect and simulated changes have been corrected for remaining model-data differences in this region. Aragonite undersaturation in Arctic surface waters is projected to occur locally within a decade and to become more widespread as atmospheric CO 2 continues to grow. The results imply that surface waters in the Arctic Ocean will become corrosive to aragonite, with potentially large implications for the marine ecosystem, if anthropogenic carbon emissions are not reduced and atmospheric CO 2 not kept below 450 ppm.
format Article in Journal/Newspaper
author M. Steinacher
F. Joos
T. L. Frölicher
G.-K. Plattner
S. C. Doney
author_facet M. Steinacher
F. Joos
T. L. Frölicher
G.-K. Plattner
S. C. Doney
author_sort M. Steinacher
title Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
title_short Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
title_full Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
title_fullStr Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
title_full_unstemmed Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
title_sort imminent ocean acidification in the arctic projected with the ncar global coupled carbon cycle-climate model
publisher Copernicus Publications
publishDate 2009
url https://doaj.org/article/a89ccdb47fce436cb17da2a9fe80b782
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Climate change
Ocean acidification
Sea ice
genre_facet Arctic
Arctic Ocean
Climate change
Ocean acidification
Sea ice
op_source Biogeosciences, Vol 6, Iss 4, Pp 515-533 (2009)
op_relation http://www.biogeosciences.net/6/515/2009/bg-6-515-2009.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
1726-4170
1726-4189
https://doaj.org/article/a89ccdb47fce436cb17da2a9fe80b782
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