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Total ozone column derived from GOME and SCIAMACHY using KNMI retrieval algorithms: Validation against Brewer measurements at the Iberian Peninsula
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dc.contributor.authorAntón, Manueles_ES
dc.contributor.authorKroon, Markes_ES
dc.contributor.authorLópez Bartolomé, Maríaes_ES
dc.contributor.authorVilaplana Guerrero, José Manueles_ES
dc.contributor.authorBañón García, Manueles_ES
dc.contributor.authorVan der A, Ronaldes_ES
dc.contributor.authorVeefkind, J. P.es_ES
dc.contributor.authorStammes, Pietes_ES
dc.contributor.authorAlados Arboledas, Lucases_ES
dc.date.accessioned2017-08-02T07:24:47Z-
dc.date.available2017-08-02T07:24:47Z-
dc.date.issued2011-
dc.identifier.citationJournal of Geophysical Research: Atmospheres. 2011, 116(D22), p. 1-13es_ES
dc.identifier.issn2169-897X-
dc.identifier.issn2169-8996-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/7372-
dc.description.abstractThis article focuses on the validation of the total ozone column (TOC) data set acquired by the Global Ozone Monitoring Experiment (GOME) and the Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) satellite remote sensing instruments using the Total Ozone Retrieval Scheme for the GOME Instrument Based on the Ozone Monitoring Instrument (TOGOMI) and Total Ozone Retrieval Scheme for the SCIAMACHY Instrument Based on the Ozone Monitoring Instrument (TOSOMI) retrieval algorithms developed by the Royal Netherlands Meteorological Institute. In this analysis, spatially colocated, daily averaged ground-based observations performed by five well-calibrated Brewer spectrophotometers at the Iberian Peninsula are used. The period of study runs from January 2004 to December 2009. The agreement between satellite and ground-based TOC data is excellent (R2 higher than 0.94). Nevertheless, the TOC data derived from both satellite instruments underestimate the ground-based data. On average, this underestimation is 1.1% for GOME and 1.3% for SCIAMACHY. The SCIAMACHY-Brewer TOC differences show a significant solar zenith angle (SZA) dependence which causes a systematic seasonal dependence. By contrast, GOME-Brewer TOC differences show no significant SZA dependence and hence no seasonality although processed with exactly the same algorithm. The satellite-Brewer TOC differences for the two satellite instruments show a clear and similar dependence on the viewing zenith angle under cloudy conditions. In addition, both the GOME-Brewer and SCIAMACHY-Brewer TOC differences reveal a very similar behavior with respect to the satellite cloud properties, being cloud fraction and cloud top pressure, which originate from the same cloud algorithm (Fast Retrieval Scheme for Clouds from the Oxygen A-Band (FRESCO+)) in both the TOSOMI and TOGOMI retrieval algorithms.es_ES
dc.description.sponsorshipThis work was partially supported by the Andalusian Regional Government through projects P08‐RNM ‐3568 andP10‐RNM‐6299, the Spanish Ministry of Science and Technology throughprojects CGL2010–18782 and CSD2007–00067, and the European Unionthrough ACTRIS project (EU INFRA‐2010‐1.1.16‐262254).es_ES
dc.language.isoenges_ES
dc.publisherWileyes_ES
dc.subjectGOMEes_ES
dc.subjectSCIAMACHYes_ES
dc.subjectTotal ozonees_ES
dc.subjectValidationes_ES
dc.titleTotal ozone column derived from GOME and SCIAMACHY using KNMI retrieval algorithms: Validation against Brewer measurements at the Iberian Peninsulaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://dx.doi.org/10.1029/2011JD016436es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/FP7/262254es_ES
Colecciones: Artículos científicos 2010-2014


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