Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol
Chlorine- and bromine-containing ozone-depleting substances (ODSs) are controlled by the 1987 Montreal Protocol. In consequence, atmospheric equivalent chlorine peaked in 1993 and has been declining slowly since then. Consistent with this, models project a gradual increase in stratospheric ozone wit...
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ftleedsuniv:oai:eprints.whiterose.ac.uk:86454 2023-05-15T13:44:51+02:00 Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol Chipperfield, MP Dhomse, SS Feng, W McKenzie, RL Velders, GJM Pyle, JA 2015-05-26 text https://eprints.whiterose.ac.uk/86454/ https://eprints.whiterose.ac.uk/86454/7/ncomms8233.pdf https://doi.org/10.1038/ncomms8233 en eng Nature Publishing Group https://eprints.whiterose.ac.uk/86454/7/ncomms8233.pdf Chipperfield, MP orcid.org/0000-0002-6803-4149 , Dhomse, SS orcid.org/0000-0003-3854-5383 , Feng, W orcid.org/0000-0002-9907-9120 et al. (3 more authors) (2015) Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol. Nature Communications, 6. 7233. ISSN 2041-1723 cc_by_4 CC-BY Article PeerReviewed 2015 ftleedsuniv https://doi.org/10.1038/ncomms8233 2023-01-30T21:32:56Z Chlorine- and bromine-containing ozone-depleting substances (ODSs) are controlled by the 1987 Montreal Protocol. In consequence, atmospheric equivalent chlorine peaked in 1993 and has been declining slowly since then. Consistent with this, models project a gradual increase in stratospheric ozone with the Antarctic ozone hole expected to disappear by ∼2050. However, we show that by 2013 the Montreal Protocol had already achieved significant benefits for the ozone layer. Using a 3D atmospheric chemistry transport model, we demonstrate that much larger ozone depletion than observed has been avoided by the protocol, with beneficial impacts on surface ultraviolet. A deep Arctic ozone hole, with column values <120 DU, would have occurred given meteorological conditions in 2011. The Antarctic ozone hole would have grown in size by 40% by 2013, with enhanced loss at subpolar latitudes. The decline over northern hemisphere middle latitudes would have continued, more than doubling to ∼15% by 2013. Article in Journal/Newspaper Antarc* Antarctic Arctic White Rose Research Online (Universities of Leeds, Sheffield & York) Arctic Antarctic The Antarctic Nature Communications 6 1 |
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White Rose Research Online (Universities of Leeds, Sheffield & York) |
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English |
description |
Chlorine- and bromine-containing ozone-depleting substances (ODSs) are controlled by the 1987 Montreal Protocol. In consequence, atmospheric equivalent chlorine peaked in 1993 and has been declining slowly since then. Consistent with this, models project a gradual increase in stratospheric ozone with the Antarctic ozone hole expected to disappear by ∼2050. However, we show that by 2013 the Montreal Protocol had already achieved significant benefits for the ozone layer. Using a 3D atmospheric chemistry transport model, we demonstrate that much larger ozone depletion than observed has been avoided by the protocol, with beneficial impacts on surface ultraviolet. A deep Arctic ozone hole, with column values <120 DU, would have occurred given meteorological conditions in 2011. The Antarctic ozone hole would have grown in size by 40% by 2013, with enhanced loss at subpolar latitudes. The decline over northern hemisphere middle latitudes would have continued, more than doubling to ∼15% by 2013. |
format |
Article in Journal/Newspaper |
author |
Chipperfield, MP Dhomse, SS Feng, W McKenzie, RL Velders, GJM Pyle, JA |
spellingShingle |
Chipperfield, MP Dhomse, SS Feng, W McKenzie, RL Velders, GJM Pyle, JA Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol |
author_facet |
Chipperfield, MP Dhomse, SS Feng, W McKenzie, RL Velders, GJM Pyle, JA |
author_sort |
Chipperfield, MP |
title |
Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol |
title_short |
Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol |
title_full |
Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol |
title_fullStr |
Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol |
title_full_unstemmed |
Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol |
title_sort |
quantifying the ozone and ultraviolet benefits already achieved by the montreal protocol |
publisher |
Nature Publishing Group |
publishDate |
2015 |
url |
https://eprints.whiterose.ac.uk/86454/ https://eprints.whiterose.ac.uk/86454/7/ncomms8233.pdf https://doi.org/10.1038/ncomms8233 |
geographic |
Arctic Antarctic The Antarctic |
geographic_facet |
Arctic Antarctic The Antarctic |
genre |
Antarc* Antarctic Arctic |
genre_facet |
Antarc* Antarctic Arctic |
op_relation |
https://eprints.whiterose.ac.uk/86454/7/ncomms8233.pdf Chipperfield, MP orcid.org/0000-0002-6803-4149 , Dhomse, SS orcid.org/0000-0003-3854-5383 , Feng, W orcid.org/0000-0002-9907-9120 et al. (3 more authors) (2015) Quantifying the ozone and ultraviolet benefits already achieved by the Montreal Protocol. Nature Communications, 6. 7233. ISSN 2041-1723 |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/ncomms8233 |
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Nature Communications |
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6 |
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1 |
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1766207652062298112 |