Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization
Termination effects of large‐scale Artificial Ocean Alkalinization (AOA) have received little attention because AOA was assumed to pose low environmental risk. With the Max‐Planck‐Institute Earth System Model, we use emission‐driven AOA simulations following the Representative Concentration Pathway...
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ftpubman:oai:pure.mpg.de:item_2558215 2023-08-27T04:11:18+02:00 Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization Ferrer-Gonzalez, M. Ilyina, T. Sonntag, S. Schmidt, H. 2018-07 application/pdf http://hdl.handle.net/21.11116/0000-0000-CF27-C http://hdl.handle.net/21.11116/0000-0002-048C-C eng eng info:eu-repo/semantics/altIdentifier/doi/10.1029/2018GL077847 http://hdl.handle.net/21.11116/0000-0000-CF27-C http://hdl.handle.net/21.11116/0000-0002-048C-C info:eu-repo/semantics/openAccess Geophysical Research Letters info:eu-repo/semantics/article 2018 ftpubman https://doi.org/10.1029/2018GL077847 2023-08-02T01:33:57Z Termination effects of large‐scale Artificial Ocean Alkalinization (AOA) have received little attention because AOA was assumed to pose low environmental risk. With the Max‐Planck‐Institute Earth System Model, we use emission‐driven AOA simulations following the Representative Concentration Pathway 8.5 (RCP8.5). We find that after termination of AOA warming trends in regions of the Northern hemisphere become ∼50% higher than those in RCP8.5 with rates similar to those caused by termination of solar geoengineering over the following three decades after cessation (up to 0.15 K/year). Rates of ocean acidification after termination of AOA outpace those in RCP8.5. In warm shallow regions where vulnerable coral reefs are located, decreasing trends in surface pH double (0.01 units/year) and the drop in the carbonate saturation state (Ω) becomes up to one order of magnitude larger (0.2 units/year). Thus, termination of AOA poses higher risks to biological systems sensitive to fast‐paced environmental changes than previously thought. Article in Journal/Newspaper Ocean acidification Max Planck Society: MPG.PuRe Geophysical Research Letters 45 14 7120 7129 |
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Max Planck Society: MPG.PuRe |
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English |
description |
Termination effects of large‐scale Artificial Ocean Alkalinization (AOA) have received little attention because AOA was assumed to pose low environmental risk. With the Max‐Planck‐Institute Earth System Model, we use emission‐driven AOA simulations following the Representative Concentration Pathway 8.5 (RCP8.5). We find that after termination of AOA warming trends in regions of the Northern hemisphere become ∼50% higher than those in RCP8.5 with rates similar to those caused by termination of solar geoengineering over the following three decades after cessation (up to 0.15 K/year). Rates of ocean acidification after termination of AOA outpace those in RCP8.5. In warm shallow regions where vulnerable coral reefs are located, decreasing trends in surface pH double (0.01 units/year) and the drop in the carbonate saturation state (Ω) becomes up to one order of magnitude larger (0.2 units/year). Thus, termination of AOA poses higher risks to biological systems sensitive to fast‐paced environmental changes than previously thought. |
format |
Article in Journal/Newspaper |
author |
Ferrer-Gonzalez, M. Ilyina, T. Sonntag, S. Schmidt, H. |
spellingShingle |
Ferrer-Gonzalez, M. Ilyina, T. Sonntag, S. Schmidt, H. Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
author_facet |
Ferrer-Gonzalez, M. Ilyina, T. Sonntag, S. Schmidt, H. |
author_sort |
Ferrer-Gonzalez, M. |
title |
Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
title_short |
Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
title_full |
Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
title_fullStr |
Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
title_full_unstemmed |
Enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
title_sort |
enhanced rates of regional warming and ocean acidification after termination of large-scale ocean alkalinization |
publishDate |
2018 |
url |
http://hdl.handle.net/21.11116/0000-0000-CF27-C http://hdl.handle.net/21.11116/0000-0002-048C-C |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Geophysical Research Letters |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2018GL077847 http://hdl.handle.net/21.11116/0000-0000-CF27-C http://hdl.handle.net/21.11116/0000-0002-048C-C |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2018GL077847 |
container_title |
Geophysical Research Letters |
container_volume |
45 |
container_issue |
14 |
container_start_page |
7120 |
op_container_end_page |
7129 |
_version_ |
1775353966101528576 |