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Aerosol Lidar observations and model calculations of the Planetary Boundary Layer evolution over Greece, during the March 2006 Total Solar Eclipse

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dc.contributor.author Amiridis, V en
dc.contributor.author Melas, D en
dc.contributor.author Balis, DS en
dc.contributor.author Papayannis, A en
dc.contributor.author Founda, D en
dc.contributor.author Katragkou, E en
dc.contributor.author Giannakaki, E en
dc.contributor.author Mamouri, RE en
dc.contributor.author Gerasopoulos, E en
dc.contributor.author Zerefos, C en
dc.date.accessioned 2014-03-01T01:25:53Z
dc.date.available 2014-03-01T01:25:53Z
dc.date.issued 2007 en
dc.identifier.issn 1680-7316 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/17788
dc.subject Air Quality Model en
dc.subject Convective Heat Transfer en
dc.subject Planetary Boundary Layer en
dc.subject Vertical Mixing en
dc.subject Mixed Layer en
dc.subject Turn Off en
dc.subject Weather Research and Forecast en
dc.subject.classification Meteorology & Atmospheric Sciences en
dc.subject.other aerosol en
dc.subject.other atmospheric modeling en
dc.subject.other boundary layer en
dc.subject.other evolution en
dc.subject.other lidar en
dc.subject.other mixing en
dc.subject.other observational method en
dc.subject.other planetary atmosphere en
dc.subject.other solar eclipse en
dc.subject.other weather forecasting en
dc.subject.other Eurasia en
dc.subject.other Europe en
dc.subject.other Greece en
dc.subject.other Southern Europe en
dc.title Aerosol Lidar observations and model calculations of the Planetary Boundary Layer evolution over Greece, during the March 2006 Total Solar Eclipse en
heal.type journalArticle en
heal.identifier.primary 10.5194/acpd-7-13537-2007 en
heal.identifier.secondary http://dx.doi.org/10.5194/acpd-7-13537-2007 en
heal.language English en
heal.publicationDate 2007 en
heal.abstract An investigation of the Planetary Boundary Layer (PBL) height evolution over Greece, during the solar eclipse of 29 March 2006, is presented. Ground based observations were carried out using lidar detection and ranging devices and ground meteorological instruments, to estimate the height of the mixing layer (ML) before, during and after the solar eclipse in northern and southern parts of Greece exhibiting different sun obscuration. Data demonstrate that the solar eclipse has induced a decrease of the PBL height, indicating a suppression of turbulence activity similar to that during the sunset hours. The changes in PBL height were associated with a very shallow entrainment zone, indicating a significant weakening of the penetrative convection. Heat transfer was confined to a thinner layer above the ground. The thickness of the entrainment zone exhibited its minimum during the maximum of the eclipse, demonstrative of turbulence mechanisms suppression at that time. Model estimations of the PBL evolution were additionally conducted using the Comprehensive Air Quality Model with extensions (CAMx) coupled with the Weather Research and Forecasting model (WRF). Model-diagnosed PBL height decrease during the solar eclipse due to vertical transport decay, in agreement with the experimental findings; vertical profiles of atmospheric particles and gaseous species showed an important vertical mixing attenuation. en
heal.publisher COPERNICUS PUBLICATIONS en
heal.journalName Atmospheric Chemistry and Physics en
dc.identifier.doi 10.5194/acpd-7-13537-2007 en
dc.identifier.isi ISI:000252166500008 en
dc.identifier.volume 7 en
dc.identifier.issue 24 en
dc.identifier.spage 6181 en
dc.identifier.epage 6189 en


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