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...

Full description

Bibliographic Details
Published in:Biogeosciences
Main Authors: Steinacher, M., Joos, F., Frölicher, T. L., Plattner, G.-K., Doney, S. C.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://boris.unibe.ch/37497/1/bg-6-515-2009.pdf
https://boris.unibe.ch/37497/
id ftunivbern:oai:boris.unibe.ch:37497
record_format openpolar
spelling ftunivbern:oai:boris.unibe.ch:37497 2023-08-20T04:02:58+02:00 Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model Steinacher, M. Joos, F. Frölicher, T. L. Plattner, G.-K. Doney, S. C. 2009 application/pdf https://boris.unibe.ch/37497/1/bg-6-515-2009.pdf https://boris.unibe.ch/37497/ eng eng Copernicus Publications https://boris.unibe.ch/37497/ info:eu-repo/semantics/openAccess Steinacher, M.; Joos, F.; Frölicher, T. L.; Plattner, G.-K.; Doney, S. C. (2009). Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model. Biogeosciences, 6(4), pp. 515-533. Göttingen: Copernicus Publications 10.5194/bg-6-515-2009 <http://dx.doi.org/10.5194/bg-6-515-2009> 530 Physics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2009 ftunivbern https://doi.org/10.5194/bg-6-515-2009 2023-07-31T20:59:35Z 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 (CO2≈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 CO2 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 CO2 not kept below 450 ppm. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Climate change Ocean acidification Sea ice BORIS (Bern Open Repository and Information System, University of Bern) Arctic Arctic Ocean Biogeosciences 6 4 515 533
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 530 Physics
spellingShingle 530 Physics
Steinacher, M.
Joos, F.
Frölicher, T. L.
Plattner, G.-K.
Doney, S. C.
Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model
topic_facet 530 Physics
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 (CO2≈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 CO2 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 CO2 not kept below 450 ppm.
format Article in Journal/Newspaper
author Steinacher, M.
Joos, F.
Frölicher, T. L.
Plattner, G.-K.
Doney, S. C.
author_facet Steinacher, M.
Joos, F.
Frölicher, T. L.
Plattner, G.-K.
Doney, S. C.
author_sort Steinacher, M.
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://boris.unibe.ch/37497/1/bg-6-515-2009.pdf
https://boris.unibe.ch/37497/
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic
Arctic Ocean
Climate change
Ocean acidification
Sea ice
genre_facet Arctic
Arctic
Arctic Ocean
Climate change
Ocean acidification
Sea ice
op_source Steinacher, M.; Joos, F.; Frölicher, T. L.; Plattner, G.-K.; Doney, S. C. (2009). Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model. Biogeosciences, 6(4), pp. 515-533. Göttingen: Copernicus Publications 10.5194/bg-6-515-2009 <http://dx.doi.org/10.5194/bg-6-515-2009>
op_relation https://boris.unibe.ch/37497/
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/bg-6-515-2009
container_title Biogeosciences
container_volume 6
container_issue 4
container_start_page 515
op_container_end_page 533
_version_ 1774713474401697792