Technical Note: One year of Raman-lidar measurements in Gual Pahari EUCAARI site close to New Delhi in India – Seasonal characteristics of the aerosol vertical structure

dc.bibliographicCitation.firstPage4513eng
dc.bibliographicCitation.issue10eng
dc.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
dc.bibliographicCitation.lastPage4524eng
dc.bibliographicCitation.volume12
dc.contributor.authorKomppula, M.
dc.contributor.authorMielonen, T.
dc.contributor.authorArola, A.
dc.contributor.authorKorhonen, K.
dc.contributor.authorLihavainen, H.
dc.contributor.authorHyvärinen, A.-P.
dc.contributor.authorBaars, H.
dc.contributor.authorEngelmann, R.
dc.contributor.authorAlthausen, D.
dc.contributor.authorAnsmann, A.
dc.contributor.authorMüller, D.
dc.contributor.authorPanwar, T.S.
dc.contributor.authorHooda, R.K.
dc.contributor.authorSharma, V.P.
dc.contributor.authorKerminen, V.-M.
dc.contributor.authorLehtinen, K.E.J.
dc.contributor.authorViisanen, Y.
dc.date.accessioned2017-11-20T21:27:59Z
dc.date.available2019-06-26T17:18:20Z
dc.date.issued2012
dc.description.abstractOne year of multi-wavelength (3 backscatter + 2 extinction + 1 depolarization) Raman lidar measurements at Gual Pahari, close to New Delhi, were analysed. The data was split into four seasons: spring (March–May), summer (June–August), autumn (September–November) and winter (December–February). The vertical profiles of backscatter, extinction, and lidar ratio and their variability during each season are presented. The measurements revealed that, on average, the aerosol layer was at its highest in spring (5.5 km). In summer, the vertically averaged (between 1–3 km) backscatter and extinction coefficients had the highest averages (3.3 Mm−1 sr−1 and 142 Mm−1 at 532 nm, respectively). Aerosol concentrations were slightly higher in summer compared to other seasons, and particles were larger in size. The autumn showed the highest lidar ratio and high extinction-related Ångström exponents (AEext), indicating the presence of smaller probably absorbing particles. The winter had the lowest backscatter and extinction coefficients, but AEext was the highest, suggesting still a large amount of small particles.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1322
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/552
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-12-4513-201
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subject.ddc550eng
dc.subject.otheraerosoleng
dc.subject.otheraerosol compositioneng
dc.subject.otherbackscattereng
dc.subject.otherextinction coefficienteng
dc.subject.otherlidareng
dc.subject.otherRaman spectroscopyeng
dc.subject.otherseasonal variationeng
dc.subject.othervertical profileeng
dc.titleTechnical Note: One year of Raman-lidar measurements in Gual Pahari EUCAARI site close to New Delhi in India – Seasonal characteristics of the aerosol vertical structureeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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