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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Main Authors: Chiodo, Gabriel, id_orcid:0 000-0002-8079-6314, Polvani, Lorenzo M.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2022
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
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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