Total ozone and equatorial zonal wind

Autores
Zossi Artigas, Marta Maria; Fernandez de Campra, Patricia
Año de publicación
2010
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Spatial correlations between total column ozone observed by TOMS and equatorial zonal winds from 1979 to 2003 have been assessed. Four months and three different altitude levels have been analyzed: January and July (solstice months), April and October (equinoctial months), and 10, 30 and 50. hPa. The results are different for the months and altitudes considered. The highest correlations values appear in tropical zone at 30. hPa. The Brewer-Dobson circulation plays a key role in regulating the abundance of ozone, influenced by the quasi-biennial oscillation (QBO) circulation. Since the Brewer-Dobson is a slow circulation, correlations considering lags between one and 12 months were estimated. In this case, the highest correlations values are moving to subtropical latitudes at winter hemisphere, with different behaviors for three altitude levels considered.
Fil: Zossi Artigas, Marta Maria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina
Fil: Fernandez de Campra, Patricia. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Ciencias de la Computación; Argentina
Materia
Brewer-Dobson Circulation
Equatorial Zonal Wind
Quasi-Biennial Oscillation
Total Column Ozone
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/74778
Acceder
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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Total ozone and equatorial zonal windZossi Artigas, Marta MariaFernandez de Campra, PatriciaBrewer-Dobson CirculationEquatorial Zonal WindQuasi-Biennial OscillationTotal Column Ozonehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Spatial correlations between total column ozone observed by TOMS and equatorial zonal winds from 1979 to 2003 have been assessed. Four months and three different altitude levels have been analyzed: January and July (solstice months), April and October (equinoctial months), and 10, 30 and 50. hPa. The results are different for the months and altitudes considered. The highest correlations values appear in tropical zone at 30. hPa. The Brewer-Dobson circulation plays a key role in regulating the abundance of ozone, influenced by the quasi-biennial oscillation (QBO) circulation. Since the Brewer-Dobson is a slow circulation, correlations considering lags between one and 12 months were estimated. In this case, the highest correlations values are moving to subtropical latitudes at winter hemisphere, with different behaviors for three altitude levels considered.Fil: Zossi Artigas, Marta Maria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; ArgentinaFil: Fernandez de Campra, Patricia. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Ciencias de la Computación; ArgentinaElsevier2010-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/74778Zossi Artigas, Marta Maria; Fernandez de Campra, Patricia; Total ozone and equatorial zonal wind; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 72; 16; 10-2010; 1180-11831364-6826CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jastp.2010.07.014info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1364682610002105?via%3Dihubinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T14:51:35Zoai:ri.conicet.gov.ar:11336/74778instacron: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:34982025-10-15 14:51:35.434CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Total ozone and equatorial zonal wind
title Total ozone and equatorial zonal wind
spellingShingle Total ozone and equatorial zonal wind
Zossi Artigas, Marta Maria
Brewer-Dobson Circulation
Equatorial Zonal Wind
Quasi-Biennial Oscillation
Total Column Ozone
title_short Total ozone and equatorial zonal wind
title_full Total ozone and equatorial zonal wind
title_fullStr Total ozone and equatorial zonal wind
title_full_unstemmed Total ozone and equatorial zonal wind
title_sort Total ozone and equatorial zonal wind
dc.creator.none.fl_str_mv Zossi Artigas, Marta Maria
Fernandez de Campra, Patricia
author Zossi Artigas, Marta Maria
author_facet Zossi Artigas, Marta Maria
Fernandez de Campra, Patricia
author_role author
author2 Fernandez de Campra, Patricia
author2_role author
dc.subject.none.fl_str_mv Brewer-Dobson Circulation
Equatorial Zonal Wind
Quasi-Biennial Oscillation
Total Column Ozone
topic Brewer-Dobson Circulation
Equatorial Zonal Wind
Quasi-Biennial Oscillation
Total Column Ozone
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Spatial correlations between total column ozone observed by TOMS and equatorial zonal winds from 1979 to 2003 have been assessed. Four months and three different altitude levels have been analyzed: January and July (solstice months), April and October (equinoctial months), and 10, 30 and 50. hPa. The results are different for the months and altitudes considered. The highest correlations values appear in tropical zone at 30. hPa. The Brewer-Dobson circulation plays a key role in regulating the abundance of ozone, influenced by the quasi-biennial oscillation (QBO) circulation. Since the Brewer-Dobson is a slow circulation, correlations considering lags between one and 12 months were estimated. In this case, the highest correlations values are moving to subtropical latitudes at winter hemisphere, with different behaviors for three altitude levels considered.
Fil: Zossi Artigas, Marta Maria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina
Fil: Fernandez de Campra, Patricia. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Física; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Exactas y Tecnología. Departamento de Ciencias de la Computación; Argentina
description Spatial correlations between total column ozone observed by TOMS and equatorial zonal winds from 1979 to 2003 have been assessed. Four months and three different altitude levels have been analyzed: January and July (solstice months), April and October (equinoctial months), and 10, 30 and 50. hPa. The results are different for the months and altitudes considered. The highest correlations values appear in tropical zone at 30. hPa. The Brewer-Dobson circulation plays a key role in regulating the abundance of ozone, influenced by the quasi-biennial oscillation (QBO) circulation. Since the Brewer-Dobson is a slow circulation, correlations considering lags between one and 12 months were estimated. In this case, the highest correlations values are moving to subtropical latitudes at winter hemisphere, with different behaviors for three altitude levels considered.
publishDate 2010
dc.date.none.fl_str_mv 2010-10
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/11336/74778
Zossi Artigas, Marta Maria; Fernandez de Campra, Patricia; Total ozone and equatorial zonal wind; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 72; 16; 10-2010; 1180-1183
1364-6826
CONICET Digital
CONICET
url http://hdl.handle.net/11336/74778
identifier_str_mv Zossi Artigas, Marta Maria; Fernandez de Campra, Patricia; Total ozone and equatorial zonal wind; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 72; 16; 10-2010; 1180-1183
1364-6826
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jastp.2010.07.014
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1364682610002105?via%3Dihub
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
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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score 13.22299

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