Kinetics of the BrO + ClO reaction and implications for stratospheric ozone
The gas-phase reaction between BrO and CIO has been proposed as a potentially fast and synergistic mechanism of stratospheric ozone destruction. Further, it has been advanced1as a contributing factor to Antarctic springtime ozone column losses of ∼40% from 1960 to 19852,3Both dynamical4and chemical...
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ftcdlib:qt6h01h1ps 2023-05-15T14:04:14+02:00 Kinetics of the BrO + ClO reaction and implications for stratospheric ozone Hills, AJ Cicerone, RJ Calvert, JG Birks, JW 405 - 408 1988-12-01 application/pdf http://www.escholarship.org/uc/item/6h01h1ps english eng eScholarship, University of California qt6h01h1ps http://www.escholarship.org/uc/item/6h01h1ps Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Hills, AJ; Cicerone, RJ; Calvert, JG; & Birks, JW. (1988). Kinetics of the BrO + ClO reaction and implications for stratospheric ozone. Nature, 328(6129), 405 - 408. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/6h01h1ps article 1988 ftcdlib 2018-07-06T22:51:20Z The gas-phase reaction between BrO and CIO has been proposed as a potentially fast and synergistic mechanism of stratospheric ozone destruction. Further, it has been advanced1as a contributing factor to Antarctic springtime ozone column losses of ∼40% from 1960 to 19852,3Both dynamical4and chemical theories1,5-8have been advanced to explain the formation of the Antarctic 'ozone hole'. A major uncertainty in these theories has been the rate constant and product distribution of the BrO + ClO reaction as a function of temperature. Here we report the first direct measurements of these parameters. We show that this reaction could, indeed, account for a large fraction of the springtime ozone depletion over Antarctica and provide a source of chlorine dioxide of sufficient magnitude to explain the recent measurements of this species in the Antarctic stratosphere, provided that the stratosphere contains a sufficient quantity of bromine (∼20 p.p.t.v.). © 1987 Nature Publishing Group. Article in Journal/Newspaper Antarc* Antarctic Antarctica University of California: eScholarship Antarctic The Antarctic |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
English |
description |
The gas-phase reaction between BrO and CIO has been proposed as a potentially fast and synergistic mechanism of stratospheric ozone destruction. Further, it has been advanced1as a contributing factor to Antarctic springtime ozone column losses of ∼40% from 1960 to 19852,3Both dynamical4and chemical theories1,5-8have been advanced to explain the formation of the Antarctic 'ozone hole'. A major uncertainty in these theories has been the rate constant and product distribution of the BrO + ClO reaction as a function of temperature. Here we report the first direct measurements of these parameters. We show that this reaction could, indeed, account for a large fraction of the springtime ozone depletion over Antarctica and provide a source of chlorine dioxide of sufficient magnitude to explain the recent measurements of this species in the Antarctic stratosphere, provided that the stratosphere contains a sufficient quantity of bromine (∼20 p.p.t.v.). © 1987 Nature Publishing Group. |
format |
Article in Journal/Newspaper |
author |
Hills, AJ Cicerone, RJ Calvert, JG Birks, JW |
spellingShingle |
Hills, AJ Cicerone, RJ Calvert, JG Birks, JW Kinetics of the BrO + ClO reaction and implications for stratospheric ozone |
author_facet |
Hills, AJ Cicerone, RJ Calvert, JG Birks, JW |
author_sort |
Hills, AJ |
title |
Kinetics of the BrO + ClO reaction and implications for stratospheric ozone |
title_short |
Kinetics of the BrO + ClO reaction and implications for stratospheric ozone |
title_full |
Kinetics of the BrO + ClO reaction and implications for stratospheric ozone |
title_fullStr |
Kinetics of the BrO + ClO reaction and implications for stratospheric ozone |
title_full_unstemmed |
Kinetics of the BrO + ClO reaction and implications for stratospheric ozone |
title_sort |
kinetics of the bro + clo reaction and implications for stratospheric ozone |
publisher |
eScholarship, University of California |
publishDate |
1988 |
url |
http://www.escholarship.org/uc/item/6h01h1ps |
op_coverage |
405 - 408 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
Hills, AJ; Cicerone, RJ; Calvert, JG; & Birks, JW. (1988). Kinetics of the BrO + ClO reaction and implications for stratospheric ozone. Nature, 328(6129), 405 - 408. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/6h01h1ps |
op_relation |
qt6h01h1ps http://www.escholarship.org/uc/item/6h01h1ps |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
_version_ |
1766275263967002624 |