Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/30756
DC FieldValueLanguage
dc.contributor.authorFountoulakis, Ilias-
dc.contributor.authorBais, Alkiviadis F.-
dc.contributor.authorFragkos, Konstantinos-
dc.contributor.authorMeleti, Charickleia-
dc.contributor.authorTourpali, Kleareti D.-
dc.contributor.authorZempila, Melina Maria-
dc.date.accessioned2023-11-08T08:10:20Z-
dc.date.available2023-11-08T08:10:20Z-
dc.date.issued2016-03-01-
dc.identifier.citationAtmospheric Chemistry and Physics, vol. 16, iss. 4, pp. 2493 - 2505en_US
dc.identifier.issn16807316-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/30756-
dc.description.abstractIn this study, we discuss the short- and the long-term variability of spectral UV irradiance at Thessaloniki, Greece, using a long, quality-controlled data set from two Brewer spectrophotometers. Long-term changes in spectral UV irradiance at 307.5, 324 and 350 nm for the period 1994-2014 are presented for different solar zenith angles and discussed in association with changes in total ozone column (TOC), aerosol optical depth (AOD) and cloudiness observed in the same period. Positive changes in annual mean anomalies of UV irradiance, ranging from 2 to 6 % per decade, have been detected both for clear- and all-sky conditions. The changes are generally greater for larger solar zenith angles and for shorter wavelengths. For clear-skies, these changes are, in most cases, statistically significant at the 95 % confidence limit. Decreases in the aerosol load and weakening of the attenuation by clouds lead to increases in UV irradiance in the summer, of 7-9 % per decade for 64° solar zenith angle. The increasing TOC in winter counteracts the effect of decreasing AOD for this particular season, leading to small, statistically insignificant, negative long-term changes in irradiance at 307.5 nm. Annual mean UV irradiance levels are increasing from 1994 to 2006 and remain relatively stable thereafter, possibly due to the combined changes in the amount and optical properties of aerosols. However, no statistically significant corresponding turning point has been detected in the long-term changes of AOD. The absence of signatures of changes in AOD in the short-term variability of irradiance in the UV-A may have been caused by changes in the single scattering albedo of aerosols, which may counteract the effects of changes in AOD on irradiance. The anti-correlation between the year-to-year variability of the irradiance at 307.5 nm and TOC is clear and becomes clearer as the AOD decreases.en_US
dc.language.isoenen_US
dc.relation.ispartofAtmospheric Chemistry and Physicsen_US
dc.rights© Author(s)en_US
dc.subjectCentral Macedoniaen_US
dc.subjectGreeceen_US
dc.subjectThessalonikien_US
dc.subjectaerosol propertyen_US
dc.subjectcloud coveren_US
dc.subjectirradianceen_US
dc.subjectsolar radiationen_US
dc.subjecttotal ozoneen_US
dc.subjectultraviolet radiationen_US
dc.subjectzenith angleen_US
dc.titleShort- and long-term variability of spectral solar UV irradiance at Thessaloniki, Greece: Effects of changes in aerosols, total ozone and cloudsen_US
dc.typeArticleen_US
dc.collaborationAristotle University of Thessalonikien_US
dc.collaborationColorado State Universityen_US
dc.subject.categoryNATURAL SCIENCESen_US
dc.subject.categoryENGINEERING AND TECHNOLOGYen_US
dc.subject.categoryCivil Engineeringen_US
dc.journalsSubscriptionen_US
dc.countryGreeceen_US
dc.countryUnited Statesen_US
dc.subject.fieldNatural Sciencesen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.5194/acp-16-2493-2016en_US
dc.identifier.scopus2-s2.0-84959525197en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/84959525197en
dc.contributor.orcid#NODATA#en
dc.contributor.orcid#NODATA#en
dc.contributor.orcid#NODATA#en
dc.contributor.orcid#NODATA#en
dc.contributor.orcid#NODATA#en
dc.contributor.orcid#NODATA#en
dc.relation.issue4en_US
dc.relation.volume16en_US
cut.common.academicyear2016-2017en_US
dc.identifier.spage2493en_US
dc.identifier.epage2505en_US
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.openairetypearticle-
item.cerifentitytypePublications-
item.grantfulltextnone-
item.languageiso639-1en-
item.fulltextNo Fulltext-
crisitem.journal.journalissn1680-7324-
crisitem.journal.publisherEuropean Geosciences Union-
crisitem.author.orcid0000-0002-3009-2407-
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