Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century

Autores
Fernandez, Rafael Pedro; Kinnison, Douglas E.; Lamarque, Jean Francois; Tilmes, Simone; Saiz-lopez, Alfonso
Año de publicación
2017
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Active bromine released from the photochemical decomposition of biogenic very short-lived bromocarbons (VSL_Br ) enhances stratospheric ozone depletion. Based on a dual set of 1960-2100 coupled chemistry-climate simulations (i.e. with and without VSL Br ), we show that the maximum Antarctic ozone hole depletion increases by up to 14% when natural VSLBr are considered, in better agreement with ozone observations. The impact of the additional 5 pptv VSL Br on Antarctic ozone is most evident in the periphery of the ozone hole, producing an expansion of the ozone hole area of ~5 million km 2 , which is equivalent in magnitude to the recently estimated Antarctic ozone healing due to the implementation of the Montreal Protocol. We find that the inclusion of VSL Br in CAM-Chem does not introduce a significant delay of the modelled ozone return date to 1980 October levels, but instead affect the depth and duration of the simulated ozone hole. Our analysis further shows that total bromine-catalysed ozone destruction in the lower stratosphere surpasses that of chlorine by year 2070, and indicates that natural VSL Br chemistry would dominate Antarctic ozone seasonality before the end of the 21 st century. This work suggests a large influence of biogenic bromine on the future Antarctic ozone layer.
Fil: Fernandez, Rafael Pedro. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España. Universidad Tecnologica Nacional. Facultad Regional Mendoza. Secretaría de Ciencia, Tecnología y Postgrado; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina
Fil: Kinnison, Douglas E.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Lamarque, Jean Francois. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Tilmes, Simone. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Saiz-lopez, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España
Materia
VSL BROMINE
ANTARCTIC OZONE HOLE
OZONE RECOVERY DATE
OZONE HOLE AREA
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/100402

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spelling Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st centuryFernandez, Rafael PedroKinnison, Douglas E.Lamarque, Jean FrancoisTilmes, SimoneSaiz-lopez, AlfonsoVSL BROMINEANTARCTIC OZONE HOLEOZONE RECOVERY DATEOZONE HOLE AREAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Active bromine released from the photochemical decomposition of biogenic very short-lived bromocarbons (VSL_Br ) enhances stratospheric ozone depletion. Based on a dual set of 1960-2100 coupled chemistry-climate simulations (i.e. with and without VSL Br ), we show that the maximum Antarctic ozone hole depletion increases by up to 14% when natural VSLBr are considered, in better agreement with ozone observations. The impact of the additional 5 pptv VSL Br on Antarctic ozone is most evident in the periphery of the ozone hole, producing an expansion of the ozone hole area of ~5 million km 2 , which is equivalent in magnitude to the recently estimated Antarctic ozone healing due to the implementation of the Montreal Protocol. We find that the inclusion of VSL Br in CAM-Chem does not introduce a significant delay of the modelled ozone return date to 1980 October levels, but instead affect the depth and duration of the simulated ozone hole. Our analysis further shows that total bromine-catalysed ozone destruction in the lower stratosphere surpasses that of chlorine by year 2070, and indicates that natural VSL Br chemistry would dominate Antarctic ozone seasonality before the end of the 21 st century. This work suggests a large influence of biogenic bromine on the future Antarctic ozone layer.Fil: Fernandez, Rafael Pedro. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España. Universidad Tecnologica Nacional. Facultad Regional Mendoza. Secretaría de Ciencia, Tecnología y Postgrado; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; ArgentinaFil: Kinnison, Douglas E.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados UnidosFil: Lamarque, Jean Francois. National Center For Atmospheric Research. Amospheric Chemistry División; Estados UnidosFil: Tilmes, Simone. National Center For Atmospheric Research. Amospheric Chemistry División; Estados UnidosFil: Saiz-lopez, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; EspañaCopernicus Publications2017-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/100402Fernandez, Rafael Pedro; Kinnison, Douglas E.; Lamarque, Jean Francois; Tilmes, Simone; Saiz-lopez, Alfonso; Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century; Copernicus Publications; Atmospheric Chemistry and Physics; 1-2017; 1-271680-73161680-7324CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.5194/acp-2016-840info:eu-repo/semantics/altIdentifier/url/https://www.atmos-chem-phys.net/17/1673/2017/info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:14:55Zoai:ri.conicet.gov.ar:11336/100402instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-10 13:14:55.391CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
title Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
spellingShingle Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
Fernandez, Rafael Pedro
VSL BROMINE
ANTARCTIC OZONE HOLE
OZONE RECOVERY DATE
OZONE HOLE AREA
title_short Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
title_full Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
title_fullStr Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
title_full_unstemmed Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
title_sort Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century
dc.creator.none.fl_str_mv Fernandez, Rafael Pedro
Kinnison, Douglas E.
Lamarque, Jean Francois
Tilmes, Simone
Saiz-lopez, Alfonso
author Fernandez, Rafael Pedro
author_facet Fernandez, Rafael Pedro
Kinnison, Douglas E.
Lamarque, Jean Francois
Tilmes, Simone
Saiz-lopez, Alfonso
author_role author
author2 Kinnison, Douglas E.
Lamarque, Jean Francois
Tilmes, Simone
Saiz-lopez, Alfonso
author2_role author
author
author
author
dc.subject.none.fl_str_mv VSL BROMINE
ANTARCTIC OZONE HOLE
OZONE RECOVERY DATE
OZONE HOLE AREA
topic VSL BROMINE
ANTARCTIC OZONE HOLE
OZONE RECOVERY DATE
OZONE HOLE AREA
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Active bromine released from the photochemical decomposition of biogenic very short-lived bromocarbons (VSL_Br ) enhances stratospheric ozone depletion. Based on a dual set of 1960-2100 coupled chemistry-climate simulations (i.e. with and without VSL Br ), we show that the maximum Antarctic ozone hole depletion increases by up to 14% when natural VSLBr are considered, in better agreement with ozone observations. The impact of the additional 5 pptv VSL Br on Antarctic ozone is most evident in the periphery of the ozone hole, producing an expansion of the ozone hole area of ~5 million km 2 , which is equivalent in magnitude to the recently estimated Antarctic ozone healing due to the implementation of the Montreal Protocol. We find that the inclusion of VSL Br in CAM-Chem does not introduce a significant delay of the modelled ozone return date to 1980 October levels, but instead affect the depth and duration of the simulated ozone hole. Our analysis further shows that total bromine-catalysed ozone destruction in the lower stratosphere surpasses that of chlorine by year 2070, and indicates that natural VSL Br chemistry would dominate Antarctic ozone seasonality before the end of the 21 st century. This work suggests a large influence of biogenic bromine on the future Antarctic ozone layer.
Fil: Fernandez, Rafael Pedro. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España. Universidad Tecnologica Nacional. Facultad Regional Mendoza. Secretaría de Ciencia, Tecnología y Postgrado; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina
Fil: Kinnison, Douglas E.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Lamarque, Jean Francois. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Tilmes, Simone. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Saiz-lopez, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España
description Active bromine released from the photochemical decomposition of biogenic very short-lived bromocarbons (VSL_Br ) enhances stratospheric ozone depletion. Based on a dual set of 1960-2100 coupled chemistry-climate simulations (i.e. with and without VSL Br ), we show that the maximum Antarctic ozone hole depletion increases by up to 14% when natural VSLBr are considered, in better agreement with ozone observations. The impact of the additional 5 pptv VSL Br on Antarctic ozone is most evident in the periphery of the ozone hole, producing an expansion of the ozone hole area of ~5 million km 2 , which is equivalent in magnitude to the recently estimated Antarctic ozone healing due to the implementation of the Montreal Protocol. We find that the inclusion of VSL Br in CAM-Chem does not introduce a significant delay of the modelled ozone return date to 1980 October levels, but instead affect the depth and duration of the simulated ozone hole. Our analysis further shows that total bromine-catalysed ozone destruction in the lower stratosphere surpasses that of chlorine by year 2070, and indicates that natural VSL Br chemistry would dominate Antarctic ozone seasonality before the end of the 21 st century. This work suggests a large influence of biogenic bromine on the future Antarctic ozone layer.
publishDate 2017
dc.date.none.fl_str_mv 2017-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/100402
Fernandez, Rafael Pedro; Kinnison, Douglas E.; Lamarque, Jean Francois; Tilmes, Simone; Saiz-lopez, Alfonso; Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century; Copernicus Publications; Atmospheric Chemistry and Physics; 1-2017; 1-27
1680-7316
1680-7324
CONICET Digital
CONICET
url http://hdl.handle.net/11336/100402
identifier_str_mv Fernandez, Rafael Pedro; Kinnison, Douglas E.; Lamarque, Jean Francois; Tilmes, Simone; Saiz-lopez, Alfonso; Impact of biogenic very short-lived bromine on the Antarctic ozone hole during the 21st century; Copernicus Publications; Atmospheric Chemistry and Physics; 1-2017; 1-27
1680-7316
1680-7324
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-2016-840
info:eu-repo/semantics/altIdentifier/url/https://www.atmos-chem-phys.net/17/1673/2017/
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Copernicus Publications
publisher.none.fl_str_mv Copernicus Publications
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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