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dc.contributor.author
Wolfram, Elian Augusto  
dc.contributor.author
Salvador, Jacobo Omar  
dc.contributor.author
Orte, Pablo Facundo  
dc.contributor.author
D'elia, Raul Luis  
dc.contributor.author
Godin Beekmann, S.  
dc.contributor.author
Kuttippurath, J.  
dc.contributor.author
Pazmiño, A.  
dc.contributor.author
Goutail, F.  
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Casiccia, C.  
dc.contributor.author
Zamorano, F.  
dc.contributor.author
Paes Leme, N.  
dc.contributor.author
Quel, Eduardo Jaime  
dc.date.available
2019-08-20T19:18:11Z  
dc.date.issued
2012-07  
dc.identifier.citation
Wolfram, Elian Augusto; Salvador, Jacobo Omar; Orte, Pablo Facundo; D'elia, Raul Luis; Godin Beekmann, S.; et al.; The unusual persistence of an ozone hole over a southern mid-latitude station during the Antarctic spring 2009: A multi-instrument study; Copernicus Publications; Annales Geophysicae; 30; 10; 7-2012; 1435-1449  
dc.identifier.issn
0992-7689  
dc.identifier.uri
http://hdl.handle.net/11336/81846  
dc.description.abstract
Record-low ozone column densities (with a minimum of 212 DU) persisted over three weeks at the Río Gallegos NDACC (Network for the Detection of Atmospheric Composition Change) station (51.5° S, 69.3° W) in November 2009. Total ozone remained two standard deviations below the climatological mean for five consecutive days during this period. The statistical analysis of 30 years of satellite data from the Multi Sensor Reanalysis (MSR) database for Río Gallegos revealed that such a long-lasting low-ozone episode is a rare occurrence. The event is examined using height-resolved ozone lidar measurements at Río Gallegos, and observations from satellite and groundbased instruments. The computed relative difference between the measured total ozone and the climatological monthly mean shows reductions varying between 10 and 30% with an average decrease of 25 %. The mean absolute difference of total ozone column with respect to climatological monthly mean ozone column is around 75 DU. Extreme values of the UV index (UVI) were measured at the ground for this period, with the daily maximum UVI of around 13 on 15 and 28 November. The high-resolution MIMOSACHIM (Modélisation Isentrope du transport Méso-échelle de l'Ozone Stratosphérique par Advection) model was used to interpret the ozone depletion event. An ozone decrease of about 2 ppmv was observed in mid-November at the 550K isentropic level (~22 km). The position of Río Gallegos relative to the polar vortex was classified using equivalent latitude maps. During the second week of November, the vortex was over the station at all isentropic levels, but after 20 November and until the end of the month, only the 10 lower levels in the stratosphere were affected by vortex overpasses with ozone poor air masses. A rapid recovery of the ozone column density was observed later, due to an ozone rich filament moving over Río Gallegos between 18 and 24 km in the first two weeks of December 2009.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Copernicus Publications  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Atmospheric Composition And Structure (Middle Atmosphere - Composition And Chemistry)  
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Meteorología y Ciencias Atmosféricas  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
The unusual persistence of an ozone hole over a southern mid-latitude station during the Antarctic spring 2009: A multi-instrument study  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2019-08-16T18:41:08Z  
dc.identifier.eissn
1432-0576  
dc.journal.volume
30  
dc.journal.number
10  
dc.journal.pagination
1435-1449  
dc.journal.pais
Alemania  
dc.journal.ciudad
Gottingen  
dc.description.fil
Fil: Wolfram, Elian Augusto. Consejo Nacional de Investigaciones Científicas y Técnicas. Unidad de Investigación y Desarrollo Estratégico para la Defensa. Ministerio de Defensa. Unidad de Investigación y Desarrollo Estratégico para la Defensa; Argentina  
dc.description.fil
Fil: Salvador, Jacobo Omar. Consejo Nacional de Investigaciones Científicas y Técnicas. Unidad de Investigación y Desarrollo Estratégico para la Defensa. Ministerio de Defensa. Unidad de Investigación y Desarrollo Estratégico para la Defensa; Argentina  
dc.description.fil
Fil: Orte, Pablo Facundo. Consejo Nacional de Investigaciones Científicas y Técnicas. Unidad de Investigación y Desarrollo Estratégico para la Defensa. Ministerio de Defensa. Unidad de Investigación y Desarrollo Estratégico para la Defensa; Argentina  
dc.description.fil
Fil: D'elia, Raul Luis. Consejo Nacional de Investigaciones Científicas y Técnicas. Unidad de Investigación y Desarrollo Estratégico para la Defensa. Ministerio de Defensa. Unidad de Investigación y Desarrollo Estratégico para la Defensa; Argentina  
dc.description.fil
Fil: Godin Beekmann, S.. Centre National de la Recherche Scientifique; Francia  
dc.description.fil
Fil: Kuttippurath, J.. Centre National de la Recherche Scientifique; Francia  
dc.description.fil
Fil: Pazmiño, A.. Centre National de la Recherche Scientifique; Francia  
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Fil: Goutail, F.. Centre National de la Recherche Scientifique; Francia  
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Fil: Casiccia, C.. Universidad de Magallanes; Chile  
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Fil: Zamorano, F.. Universidad de Magallanes; Chile  
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Fil: Paes Leme, N.. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil  
dc.description.fil
Fil: Quel, Eduardo Jaime. Consejo Nacional de Investigaciones Científicas y Técnicas. Unidad de Investigación y Desarrollo Estratégico para la Defensa. Ministerio de Defensa. Unidad de Investigación y Desarrollo Estratégico para la Defensa; Argentina  
dc.journal.title
Annales Geophysicae  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.5194/angeo-30-1435-2012  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.ann-geophys.net/30/1435/2012/