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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/32539
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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 |
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1844613210958725120 |
score |
13.070432 |