Irreversible climate change due to carbon dioxide emissions
The severity of damaging human-induced climate change depends not only on the magnitude of the change but also on the potential for irreversibility. This paper shows that the climate change that takes place due to increases in carbon dioxide concentration is largely irreversible for 1,000 years afte...
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ftpubmed:oai:pubmedcentral.nih.gov:2632717 2023-05-15T16:41:03+02:00 Irreversible climate change due to carbon dioxide emissions Solomon, Susan Plattner, Gian-Kasper Knutti, Reto Friedlingstein, Pierre 2009-02-10 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2632717 http://www.ncbi.nlm.nih.gov/pubmed/19179281 https://doi.org/10.1073/pnas.0812721106 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2632717 http://www.ncbi.nlm.nih.gov/pubmed/19179281 http://dx.doi.org/10.1073/pnas.0812721106 © 2009 by The National Academy of Sciences of the USA Freely available online through the PNAS open access option. Physical Sciences Text 2009 ftpubmed https://doi.org/10.1073/pnas.0812721106 2013-09-02T10:19:55Z The severity of damaging human-induced climate change depends not only on the magnitude of the change but also on the potential for irreversibility. This paper shows that the climate change that takes place due to increases in carbon dioxide concentration is largely irreversible for 1,000 years after emissions stop. Following cessation of emissions, removal of atmospheric carbon dioxide decreases radiative forcing, but is largely compensated by slower loss of heat to the ocean, so that atmospheric temperatures do not drop significantly for at least 1,000 years. Among illustrative irreversible impacts that should be expected if atmospheric carbon dioxide concentrations increase from current levels near 385 parts per million by volume (ppmv) to a peak of 450–600 ppmv over the coming century are irreversible dry-season rainfall reductions in several regions comparable to those of the “dust bowl” era and inexorable sea level rise. Thermal expansion of the warming ocean provides a conservative lower limit to irreversible global average sea level rise of at least 0.4–1.0 m if 21st century CO2 concentrations exceed 600 ppmv and 0.6–1.9 m for peak CO2 concentrations exceeding ≈1,000 ppmv. Additional contributions from glaciers and ice sheet contributions to future sea level rise are uncertain but may equal or exceed several meters over the next millennium or longer. Text Ice Sheet PubMed Central (PMC) Proceedings of the National Academy of Sciences 106 6 1704 1709 |
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Physical Sciences Solomon, Susan Plattner, Gian-Kasper Knutti, Reto Friedlingstein, Pierre Irreversible climate change due to carbon dioxide emissions |
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Physical Sciences |
description |
The severity of damaging human-induced climate change depends not only on the magnitude of the change but also on the potential for irreversibility. This paper shows that the climate change that takes place due to increases in carbon dioxide concentration is largely irreversible for 1,000 years after emissions stop. Following cessation of emissions, removal of atmospheric carbon dioxide decreases radiative forcing, but is largely compensated by slower loss of heat to the ocean, so that atmospheric temperatures do not drop significantly for at least 1,000 years. Among illustrative irreversible impacts that should be expected if atmospheric carbon dioxide concentrations increase from current levels near 385 parts per million by volume (ppmv) to a peak of 450–600 ppmv over the coming century are irreversible dry-season rainfall reductions in several regions comparable to those of the “dust bowl” era and inexorable sea level rise. Thermal expansion of the warming ocean provides a conservative lower limit to irreversible global average sea level rise of at least 0.4–1.0 m if 21st century CO2 concentrations exceed 600 ppmv and 0.6–1.9 m for peak CO2 concentrations exceeding ≈1,000 ppmv. Additional contributions from glaciers and ice sheet contributions to future sea level rise are uncertain but may equal or exceed several meters over the next millennium or longer. |
format |
Text |
author |
Solomon, Susan Plattner, Gian-Kasper Knutti, Reto Friedlingstein, Pierre |
author_facet |
Solomon, Susan Plattner, Gian-Kasper Knutti, Reto Friedlingstein, Pierre |
author_sort |
Solomon, Susan |
title |
Irreversible climate change due to carbon dioxide emissions |
title_short |
Irreversible climate change due to carbon dioxide emissions |
title_full |
Irreversible climate change due to carbon dioxide emissions |
title_fullStr |
Irreversible climate change due to carbon dioxide emissions |
title_full_unstemmed |
Irreversible climate change due to carbon dioxide emissions |
title_sort |
irreversible climate change due to carbon dioxide emissions |
publisher |
National Academy of Sciences |
publishDate |
2009 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2632717 http://www.ncbi.nlm.nih.gov/pubmed/19179281 https://doi.org/10.1073/pnas.0812721106 |
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Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2632717 http://www.ncbi.nlm.nih.gov/pubmed/19179281 http://dx.doi.org/10.1073/pnas.0812721106 |
op_rights |
© 2009 by The National Academy of Sciences of the USA Freely available online through the PNAS open access option. |
op_doi |
https://doi.org/10.1073/pnas.0812721106 |
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Proceedings of the National Academy of Sciences |
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106 |
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6 |
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1704 |
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1709 |
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1766031489051394048 |