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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Published in:Proceedings of the National Academy of Sciences
Main Authors: Solomon, Susan, Plattner, Gian-Kasper, Knutti, Reto, Friedlingstein, Pierre
Format: Text
Language:English
Published: National Academy of Sciences 2009
Subjects:
Online Access: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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spelling 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
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Physical Sciences
spellingShingle Physical Sciences
Solomon, Susan
Plattner, Gian-Kasper
Knutti, Reto
Friedlingstein, Pierre
Irreversible climate change due to carbon dioxide emissions
topic_facet 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
genre 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
container_title Proceedings of the National Academy of Sciences
container_volume 106
container_issue 6
container_start_page 1704
op_container_end_page 1709
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