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Systematic lidar observations of Saharan dust over Europe in the frame of EARLINET (2000-2002)

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dc.contributor.author Papayannis, A en
dc.contributor.author Amiridis, V en
dc.contributor.author Mona, L en
dc.contributor.author Tsaknakis, G en
dc.contributor.author Balis, D en
dc.contributor.author Bosenberg, J en
dc.contributor.author Chaikovski, A en
dc.contributor.author De Tomasi, F en
dc.contributor.author Grigorov, I en
dc.contributor.author Mattis, I en
dc.contributor.author Mitev, V en
dc.contributor.author Muller, D en
dc.contributor.author Nickovic, S en
dc.contributor.author Perez, C en
dc.contributor.author Pietruczuk, A en
dc.contributor.author Pisani, G en
dc.contributor.author Ravetta, F en
dc.contributor.author Rizi, V en
dc.contributor.author Sicard, M en
dc.contributor.author Trickl, T en
dc.contributor.author Wiegner, M en
dc.contributor.author Gerding, M en
dc.contributor.author Mamouri, RE en
dc.contributor.author D'Amico, G en
dc.contributor.author Pappalardo, G en
dc.date.accessioned 2014-03-01T01:29:17Z
dc.date.available 2014-03-01T01:29:17Z
dc.date.issued 2008 en
dc.identifier.issn 0148-0227 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/19203
dc.subject Aerosol Optical Depth en
dc.subject Center of Mass en
dc.subject Linear Depolarization Ratio en
dc.subject.classification Meteorology & Atmospheric Sciences en
dc.subject.other Aerosols en
dc.subject.other Backscattering en
dc.subject.other Climate change en
dc.subject.other Dust en
dc.subject.other Optical radar en
dc.subject.other aerosol en
dc.subject.other atmospheric plume en
dc.subject.other backscatter en
dc.subject.other dust en
dc.subject.other geographical region en
dc.subject.other lidar en
dc.subject.other observational method en
dc.subject.other optical depth en
dc.subject.other wavelength en
dc.subject.other Eurasia en
dc.subject.other Europe en
dc.subject.other Southern Europe en
dc.title Systematic lidar observations of Saharan dust over Europe in the frame of EARLINET (2000-2002) en
heal.type journalArticle en
heal.identifier.primary 10.1029/2007JD009028 en
heal.identifier.secondary http://dx.doi.org/10.1029/2007JD009028 en
heal.identifier.secondary D10204 en
heal.language English en
heal.publicationDate 2008 en
heal.abstract More than 130 observation days of the horizontal and vertical extent of Saharan dust intrusions over Europe during the period May 2000 to December 2002 were studied by means of a coordinated lidar network in the frame of the European Aerosol Research Lidar Network (EARLINET). The number of dust events was greatest in late spring, summer, and early autumn periods, mainly in southern (S) and southeastern (SE) Europe. Multiple aerosol dust layers of variable thickness (300-7500 m) were observed. The center of mass of these layers was located in altitudes between 850 and 8000 m. However, the mean thickness of the dust layer typically stayed around 1500-3400 m and the corresponding mean center of mass ranged from 2500 to 6000 m. In exceptional cases, dust aerosols reached northwestern (NW), northern (N), or northeastern (NE) Europe, penetrating the geographical area located between 4°W-28°E (longitude) and 38°N-58°N (latitude). Mean aerosol optical depths (AOD), extinction-to-backscatter ratios (lidar ratios, LR), and linear depolarization ratios of desert aerosols ranged from 0.1 to 0.25 at the wavelength of 355 or 351 nm, 30 to 80 sr at 355 or 351 mn, and 10 to 25% at 532 nm, respectively, within the lofted dust plumes. In these plumes typical Saharan dust backscatter coefficients ranged from 0.5 to 2 Mm-1sr-1. Southern European stations presented higher variability of the LR values and the backscatter-related Ångström exponent. values (BRAE) :20-100 sr; BRAE: -0.5 to 3) than northern ones (LR: 30-80 sr; BRAE: -0.5 to 1). Copyright 2008 by the American Geophysical Union. en
heal.publisher AMER GEOPHYSICAL UNION en
heal.journalName Journal of Geophysical Research D: Atmospheres en
dc.identifier.doi 10.1029/2007JD009028 en
dc.identifier.isi ISI:000256358900001 en
dc.identifier.volume 113 en
dc.identifier.issue 10 en


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