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Daytime and nighttime aerosol optical depth implementation in CÆLIS
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dc.contributor.authorGonzález, Ramiroes_ES
dc.contributor.authorToledano, Carloses_ES
dc.contributor.authorRomán, Robertoes_ES
dc.contributor.authorFuertes Marrón, Davides_ES
dc.contributor.authorBerjón, Albertoes_ES
dc.contributor.authorMateos, Davides_ES
dc.contributor.authorGuirado-Fuentes, Carmenes_ES
dc.contributor.authorVelasco Merino, Cristianes_ES
dc.contributor.authorAntuña-Sánchez, Juan Carloses_ES
dc.contributor.authorCalle, Abeles_ES
dc.contributor.authorCachorro, Victoria E.es_ES
dc.contributor.authorFrutos Baraja, Ángel Máximo dees_ES
dc.date.accessioned2020-07-27T09:52:06Z-
dc.date.available2020-07-27T09:52:06Z-
dc.date.issued2020-
dc.identifier.citationGeoscientific Instrumentation, Methods and Data Systems. 2020, 9(2), p. 417–433es_ES
dc.identifier.issn2193-0856-
dc.identifier.issn2193-0864-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/12313-
dc.description.abstractThe University of Valladolid (UVa, Spain) has managed a calibration center of the AErosol RObotic NETwork (AERONET) since 2006. The CÆLIS software tool, developed by UVa, was created to manage the data generated by AERONET photometers for calibration, quality control and data processing purposes. This paper exploits the potential of this tool in order to obtain products like the aerosol optical depth (AOD) and Ångström exponent (AE), which are of high interest for atmospheric and climate studies, as well as to enhance the quality control of the instruments and data managed by CÆLIS. The AOD and cloud screening algorithms implemented in CÆLIS, both based on AERONET version 3, are described in detail. The obtained products are compared with the AERONET database. In general, the differences in daytime AOD between CÆLIS and AERONET are far below the expected uncertainty of the instrument, ranging in mean differences between −1.3×10−4 at 870 nm and 6.2×10−4 at 380 nm. The standard deviations of the differences range from 2.8×10−4 at 675 nm to 8.1×10−4 at 340 nm. The AOD and AE at nighttime calculated by CÆLIS from Moon observations are also presented, showing good continuity between day and nighttime for different locations, aerosol loads and Moon phase angles. Regarding cloud screening, around 99.9 % of the observations classified as cloud-free by CÆLIS are also assumed cloud-free by AERONET; this percentage is similar for the cases considered cloud-contaminated by both databases. The obtained results point out the capability of CÆLIS as a processing system. The AOD algorithm provides the opportunity to use this tool with other instrument types and to retrieve other aerosol products in the future. This research has been supported by the Spanish Ministry of Science and Innovation (grant no. RTI2018-097864-B-I00) and the European Union's Horizon 2020 research and innovation program (grant no. 871115).es_ES
dc.description.sponsorshipThe authors gratefully thank AERONET and PHOTONS teams for the collaboration and support. The authors thank the Spanish Ministry of Science, Innovation and Universities for the support through the ePOLAAR project (RTI2018-097864-B-I00). This research has been supported by the Spanish Ministry of Science and Innovation (grant no. RTI2018-097864-B-I00) and the European Union's Horizon 2020 research and innovation program (grant no. 871115).es_ES
dc.language.isoenges_ES
dc.publisherEuropean Geosciences Uniones_ES
dc.rightsLicencia CC: Reconocimiento CC BYes_ES
dc.subjectAERONETes_ES
dc.subjectPhotometerses_ES
dc.subjectAerosol optical depthes_ES
dc.subjectAtmospheric aerosol particleses_ES
dc.titleDaytime and nighttime aerosol optical depth implementation in CÆLISes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://dx.doi.org/10.5194/gi-9-417-2020es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/871115es_ES
Colecciones: Artículos científicos 2019-2022


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