New Insights on the Radiative Impacts of Ozone-Depleting Substances
The global warming potential of Ozone-depleting substances (ODS) has long been known to be thousands of times larger than the one of CO2, but their climate impacts as greenhouse gases, i.e. unmediated ozone depletion, has received relatively little attention. Focusing on the period 1955-2005, we her...
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2022
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/551483 https://doi.org/10.3929/ethz-b-000551483 |
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author | Chiodo, Gabriel id_orcid:0 000-0002-8079-6314 Polvani, Lorenzo M. |
author_facet | Chiodo, Gabriel id_orcid:0 000-0002-8079-6314 Polvani, Lorenzo M. |
author_sort | Chiodo, Gabriel |
collection | ETH Zürich Research Collection |
description | The global warming potential of Ozone-depleting substances (ODS) has long been known to be thousands of times larger than the one of CO2, but their climate impacts as greenhouse gases, i.e. unmediated ozone depletion, has received relatively little attention. Focusing on the period 1955-2005, we here present results from offline radiative forcing (RF) calculations from a global chemistry climate model. Using realistic distributions of ODS and consistent stratospheric ozone, we show that ODS dominate the adjusted stratospheric warming of the lower stratosphere, where CO2 has little radiative impact. We also show that the global mean RF of stratospheric ozone only cancels a fraction of the RF of ODS, leaving an important ODS contribution to anthropogenic forcing. Finally we show that the RF of ODS opposes Arctic amplification, its equator-to-pole gradient being larger than the one of CO2. ISSN:0094-8276 ISSN:1944-8007 |
format | Article in Journal/Newspaper |
genre | Arctic Global warming |
genre_facet | Arctic Global warming |
geographic | Arctic |
geographic_facet | Arctic |
id | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/551483 |
institution | Open Polar |
language | English |
op_collection_id | ftethz |
op_doi | https://doi.org/20.500.11850/55148310.3929/ethz-b-00055148310.1029/2021GL096783 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.1029/2021GL096783 info:eu-repo/semantics/altIdentifier/wos/000801842200001 info:eu-repo/grantAgreement/SNF/Ambizione/180043 http://hdl.handle.net/20.500.11850/551483 |
op_rights | info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc/4.0/ Creative Commons Attribution-NonCommercial 4.0 International |
op_source | Geophysical Research Letters, 49 (10) |
publishDate | 2022 |
publisher | American Geophysical Union |
record_format | openpolar |
spelling | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/551483 2025-03-30T15:03:15+00:00 New Insights on the Radiative Impacts of Ozone-Depleting Substances Chiodo, Gabriel id_orcid:0 000-0002-8079-6314 Polvani, Lorenzo M. 2022-05-28 application/application/pdf https://hdl.handle.net/20.500.11850/551483 https://doi.org/10.3929/ethz-b-000551483 en eng American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2021GL096783 info:eu-repo/semantics/altIdentifier/wos/000801842200001 info:eu-repo/grantAgreement/SNF/Ambizione/180043 http://hdl.handle.net/20.500.11850/551483 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc/4.0/ Creative Commons Attribution-NonCommercial 4.0 International Geophysical Research Letters, 49 (10) ozone depletion radiative forcing arctic amplification info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftethz https://doi.org/20.500.11850/55148310.3929/ethz-b-00055148310.1029/2021GL096783 2025-03-05T22:09:14Z The global warming potential of Ozone-depleting substances (ODS) has long been known to be thousands of times larger than the one of CO2, but their climate impacts as greenhouse gases, i.e. unmediated ozone depletion, has received relatively little attention. Focusing on the period 1955-2005, we here present results from offline radiative forcing (RF) calculations from a global chemistry climate model. Using realistic distributions of ODS and consistent stratospheric ozone, we show that ODS dominate the adjusted stratospheric warming of the lower stratosphere, where CO2 has little radiative impact. We also show that the global mean RF of stratospheric ozone only cancels a fraction of the RF of ODS, leaving an important ODS contribution to anthropogenic forcing. Finally we show that the RF of ODS opposes Arctic amplification, its equator-to-pole gradient being larger than the one of CO2. ISSN:0094-8276 ISSN:1944-8007 Article in Journal/Newspaper Arctic Global warming ETH Zürich Research Collection Arctic |
spellingShingle | ozone depletion radiative forcing arctic amplification Chiodo, Gabriel id_orcid:0 000-0002-8079-6314 Polvani, Lorenzo M. New Insights on the Radiative Impacts of Ozone-Depleting Substances |
title | New Insights on the Radiative Impacts of Ozone-Depleting Substances |
title_full | New Insights on the Radiative Impacts of Ozone-Depleting Substances |
title_fullStr | New Insights on the Radiative Impacts of Ozone-Depleting Substances |
title_full_unstemmed | New Insights on the Radiative Impacts of Ozone-Depleting Substances |
title_short | New Insights on the Radiative Impacts of Ozone-Depleting Substances |
title_sort | new insights on the radiative impacts of ozone-depleting substances |
topic | ozone depletion radiative forcing arctic amplification |
topic_facet | ozone depletion radiative forcing arctic amplification |
url | https://hdl.handle.net/20.500.11850/551483 https://doi.org/10.3929/ethz-b-000551483 |