HEAL DSpace

Sampling of an STT event over the Eastern Mediterranean region by lidar and electrochemical sonde

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dc.contributor.author Papayannis, A en
dc.contributor.author Balis, D en
dc.contributor.author Zanis, P en
dc.contributor.author Galani, E en
dc.contributor.author Wernli, H en
dc.contributor.author Zerefos, C en
dc.contributor.author Stohl, A en
dc.contributor.author Eckhardt, S en
dc.contributor.author Amiridis, V en
dc.date.accessioned 2014-03-01T01:23:02Z
dc.date.available 2014-03-01T01:23:02Z
dc.date.issued 2005 en
dc.identifier.issn 0992-7689 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/16779
dc.subject Atmospheric composition and structure (Evolution of the atmosphere en
dc.subject Instruments and techniques) en
dc.subject Meteorology and atmospheric dynamics (Middle atmosphere dynamics en
dc.subject Turbulence) en
dc.subject.classification Astronomy & Astrophysics en
dc.subject.classification Geosciences, Multidisciplinary en
dc.subject.classification Meteorology & Atmospheric Sciences en
dc.subject.other atmospheric chemistry en
dc.subject.other lidar en
dc.subject.other middle atmosphere en
dc.subject.other mixing ratio en
dc.subject.other ozone en
dc.subject.other troposphere en
dc.subject.other vertical profile en
dc.subject.other Mediterranean Region en
dc.subject.other Mediterranean Sea en
dc.subject.other oceanic regions en
dc.subject.other World en
dc.title Sampling of an STT event over the Eastern Mediterranean region by lidar and electrochemical sonde en
heal.type journalArticle en
heal.identifier.primary 10.5194/angeo-23-2039-2005 en
heal.identifier.secondary http://dx.doi.org/10.5194/angeo-23-2039-2005 en
heal.language English en
heal.publicationDate 2005 en
heal.abstract A two-wavelength ultraviolet (289-316 nm) ozone Differential Absorption Lidar (DIAL) system is used to perform ozone measurements in the free troposphere in the Eastern Mediterranean (Northern Greece). The ozone DIAL profiles obtained during a Stratosphere-to-Troposphere Transport (STT) event are compared to that acquired by an electrochemical ozonesonde, in the altitude range between 2 and 10 km. The measurement accuracy of these two instruments is also discussed. The mean difference between the ozone profiles obtained by the two techniques is of the order of 1.11 ppbv (1.86%), while the corresponding standard deviation is 4.69 ppbv (8.16%). A case study of an STT event which occurred on 29 November 2000 is presented and analyzed, using ozone lidar, satellite and meteorological data, as well as air mass back-trajectory analysis. During this STT event ozone mixing ratios of 55-65 ppbv were observed between 5 and 7 km height above sea level (a.s.l.). Stratospheric air was mixed with tropospheric air masses, leading to potential vorticity (PV) losses due to diabatic processes. The ozone DIAL system can be used for following STT events and small-scale mixing phenomena in the free troposphere, and for providing sequences of vertical ozone profiles in the free troposphere. © European Geosciences Union 2005. en
heal.publisher EUROPEAN GEOSCIENCES UNION en
heal.journalName Annales Geophysicae en
dc.identifier.doi 10.5194/angeo-23-2039-2005 en
dc.identifier.isi ISI:000232558900007 en
dc.identifier.volume 23 en
dc.identifier.issue 6 en
dc.identifier.spage 2039 en
dc.identifier.epage 2050 en


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