Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection

Autores
Fernandez, Rafael Pedro; Salawitch, R. J.; Kinnison, D. E.; Lamarque, J. F.; Saiz-lopez, Alfonso
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Very short-lived (VSL) bromocarbons are produced at a prodigious rate by ocean biology and these source compounds (SGVSL), together with their inorganic degradation products (PGVSL), are lofted by vigorous convection to the tropical tropopause layer (TTL). Using a state-of-the-art photochemical mechanism within a global model, we calculate annual average stratospheric injection of total bromine due to VSL sources to be 5 pptv (parts per trillion by volume), with ~ 3 pptv entering the stratosphere as PGVSL and ~ 2 pptv as SGVSL. The geographic distribution and partitioning of VSL bromine within the TTL, and its consequent stratospheric injection, is highly dependent on the oceanic flux, the strength of convection and the occurrence of heterogeneous recycling reactions. Our calculations indicate atomic Br should be the dominant inorganic species in large regions of the TTL during daytime, due to the low ozone and cold conditions of this region. We propose the existence of a "tropical ring of atomic bromine" located approximately between 15 and 19 km and between 30° N and 30° S. Daytime Br / BrO ratios of up to ~ 4 are predicted within this inhomogeneous ring in regions of highly convective transport, such as the tropical Western Pacific. Therefore, we suggest that experimental programs designed to quantify the bromine budget of the TTL and the stratospheric injection of VSL biogenic bromocarbons should include a strategy for the measurement of atomic Br during daytime as well as HOBr and BrCl during nighttime.
Fil: Fernandez, Rafael Pedro. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina
Fil: Salawitch, R. J.. University of Maryland. Department of Atmospheric and Oceanic Science; Estados Unidos
Fil: Kinnison, D. E.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Lamarque, J. F.. 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
Bromine Chemistry
Very-Short Lived species
Tropical Rings of Atomic Halogens
Tropospheric and Stratosphreic Ozone
Halocarbons
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:11336/32539

id CONICETDig_5726f0a832a601e0bd0d786f3288e37d
oai_identifier_str oai:ri.conicet.gov.ar:11336/32539
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Bromine partitioning in the tropical tropopause layer: implications for stratospheric injectionFernandez, Rafael PedroSalawitch, R. J.Kinnison, D. E.Lamarque, J. F.Saiz-lopez, AlfonsoBromine ChemistryVery-Short Lived speciesTropical Rings of Atomic HalogensTropospheric and Stratosphreic OzoneHalocarbonshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Very short-lived (VSL) bromocarbons are produced at a prodigious rate by ocean biology and these source compounds (SGVSL), together with their inorganic degradation products (PGVSL), are lofted by vigorous convection to the tropical tropopause layer (TTL). Using a state-of-the-art photochemical mechanism within a global model, we calculate annual average stratospheric injection of total bromine due to VSL sources to be 5 pptv (parts per trillion by volume), with ~ 3 pptv entering the stratosphere as PGVSL and ~ 2 pptv as SGVSL. The geographic distribution and partitioning of VSL bromine within the TTL, and its consequent stratospheric injection, is highly dependent on the oceanic flux, the strength of convection and the occurrence of heterogeneous recycling reactions. Our calculations indicate atomic Br should be the dominant inorganic species in large regions of the TTL during daytime, due to the low ozone and cold conditions of this region. We propose the existence of a "tropical ring of atomic bromine" located approximately between 15 and 19 km and between 30° N and 30° S. Daytime Br / BrO ratios of up to ~ 4 are predicted within this inhomogeneous ring in regions of highly convective transport, such as the tropical Western Pacific. Therefore, we suggest that experimental programs designed to quantify the bromine budget of the TTL and the stratospheric injection of VSL biogenic bromocarbons should include a strategy for the measurement of atomic Br during daytime as well as HOBr and BrCl during nighttime.Fil: Fernandez, Rafael Pedro. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; ArgentinaFil: Salawitch, R. J.. University of Maryland. Department of Atmospheric and Oceanic Science; Estados UnidosFil: Kinnison, D. E.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados UnidosFil: Lamarque, J. F.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados UnidosFil: Saiz-lopez, Alfonso. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; EspañaCopernicus Publications2014-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/32539Lamarque, J. F.; Saiz-lopez, Alfonso; Salawitch, R. J.; Kinnison, D. E.; Fernandez, Rafael Pedro; Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection; Copernicus Publications; Atmospheric Chemistry and Physics; 14; 24; 12-2014; 13391-134101680-73161680-7324CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.atmos-chem-phys.net/14/13391/2014/info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-14-13391-2014info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:38:19Zoai:ri.conicet.gov.ar:11336/32539instacron: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:34982025-09-29 09:38:20.116CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
title Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
spellingShingle Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
Fernandez, Rafael Pedro
Bromine Chemistry
Very-Short Lived species
Tropical Rings of Atomic Halogens
Tropospheric and Stratosphreic Ozone
Halocarbons
title_short Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
title_full Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
title_fullStr Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
title_full_unstemmed Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
title_sort Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection
dc.creator.none.fl_str_mv Fernandez, Rafael Pedro
Salawitch, R. J.
Kinnison, D. E.
Lamarque, J. F.
Saiz-lopez, Alfonso
author Fernandez, Rafael Pedro
author_facet Fernandez, Rafael Pedro
Salawitch, R. J.
Kinnison, D. E.
Lamarque, J. F.
Saiz-lopez, Alfonso
author_role author
author2 Salawitch, R. J.
Kinnison, D. E.
Lamarque, J. F.
Saiz-lopez, Alfonso
author2_role author
author
author
author
dc.subject.none.fl_str_mv Bromine Chemistry
Very-Short Lived species
Tropical Rings of Atomic Halogens
Tropospheric and Stratosphreic Ozone
Halocarbons
topic Bromine Chemistry
Very-Short Lived species
Tropical Rings of Atomic Halogens
Tropospheric and Stratosphreic Ozone
Halocarbons
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Very short-lived (VSL) bromocarbons are produced at a prodigious rate by ocean biology and these source compounds (SGVSL), together with their inorganic degradation products (PGVSL), are lofted by vigorous convection to the tropical tropopause layer (TTL). Using a state-of-the-art photochemical mechanism within a global model, we calculate annual average stratospheric injection of total bromine due to VSL sources to be 5 pptv (parts per trillion by volume), with ~ 3 pptv entering the stratosphere as PGVSL and ~ 2 pptv as SGVSL. The geographic distribution and partitioning of VSL bromine within the TTL, and its consequent stratospheric injection, is highly dependent on the oceanic flux, the strength of convection and the occurrence of heterogeneous recycling reactions. Our calculations indicate atomic Br should be the dominant inorganic species in large regions of the TTL during daytime, due to the low ozone and cold conditions of this region. We propose the existence of a "tropical ring of atomic bromine" located approximately between 15 and 19 km and between 30° N and 30° S. Daytime Br / BrO ratios of up to ~ 4 are predicted within this inhomogeneous ring in regions of highly convective transport, such as the tropical Western Pacific. Therefore, we suggest that experimental programs designed to quantify the bromine budget of the TTL and the stratospheric injection of VSL biogenic bromocarbons should include a strategy for the measurement of atomic Br during daytime as well as HOBr and BrCl during nighttime.
Fil: Fernandez, Rafael Pedro. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina
Fil: Salawitch, R. J.. University of Maryland. Department of Atmospheric and Oceanic Science; Estados Unidos
Fil: Kinnison, D. E.. National Center For Atmospheric Research. Amospheric Chemistry División; Estados Unidos
Fil: Lamarque, J. F.. 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 Very short-lived (VSL) bromocarbons are produced at a prodigious rate by ocean biology and these source compounds (SGVSL), together with their inorganic degradation products (PGVSL), are lofted by vigorous convection to the tropical tropopause layer (TTL). Using a state-of-the-art photochemical mechanism within a global model, we calculate annual average stratospheric injection of total bromine due to VSL sources to be 5 pptv (parts per trillion by volume), with ~ 3 pptv entering the stratosphere as PGVSL and ~ 2 pptv as SGVSL. The geographic distribution and partitioning of VSL bromine within the TTL, and its consequent stratospheric injection, is highly dependent on the oceanic flux, the strength of convection and the occurrence of heterogeneous recycling reactions. Our calculations indicate atomic Br should be the dominant inorganic species in large regions of the TTL during daytime, due to the low ozone and cold conditions of this region. We propose the existence of a "tropical ring of atomic bromine" located approximately between 15 and 19 km and between 30° N and 30° S. Daytime Br / BrO ratios of up to ~ 4 are predicted within this inhomogeneous ring in regions of highly convective transport, such as the tropical Western Pacific. Therefore, we suggest that experimental programs designed to quantify the bromine budget of the TTL and the stratospheric injection of VSL biogenic bromocarbons should include a strategy for the measurement of atomic Br during daytime as well as HOBr and BrCl during nighttime.
publishDate 2014
dc.date.none.fl_str_mv 2014-12
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/11336/32539
Lamarque, J. F.; Saiz-lopez, Alfonso; Salawitch, R. J.; Kinnison, D. E.; Fernandez, Rafael Pedro; Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection; Copernicus Publications; Atmospheric Chemistry and Physics; 14; 24; 12-2014; 13391-13410
1680-7316
1680-7324
CONICET Digital
CONICET
url http://hdl.handle.net/11336/32539
identifier_str_mv Lamarque, J. F.; Saiz-lopez, Alfonso; Salawitch, R. J.; Kinnison, D. E.; Fernandez, Rafael Pedro; Bromine partitioning in the tropical tropopause layer: implications for stratospheric injection; Copernicus Publications; Atmospheric Chemistry and Physics; 14; 24; 12-2014; 13391-13410
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/url/https://www.atmos-chem-phys.net/14/13391/2014/
info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-14-13391-2014
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
_version_ 1844613210958725120
score 13.070432