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dc.contributor.authorSoupiona, O.
dc.contributor.authorSamaras, S.
dc.contributor.authorOrtiz-Amezcua, Pablo
dc.contributor.authorBöckmann, C.
dc.contributor.authorPapayannis, A.
dc.contributor.authorMoreira, G.A.
dc.contributor.authorBenavent Oltra, José Antonio
dc.contributor.authorGuerrero Rascado, Juan Luis 
dc.contributor.authorBedoya-Velásquez, Andrés Esteban
dc.contributor.authorOlmo Reyes, Francisco José 
dc.contributor.authorRomán, R.
dc.contributor.authorKokkalis, P.
dc.contributor.authorMylonaki, M.
dc.contributor.authorAlados Arboledas, Lucas 
dc.contributor.authorPapanikolaou, C.A.
dc.contributor.authorFoskinis, R.
dc.date.accessioned2019-07-12T07:54:39Z
dc.date.available2019-07-12T07:54:39Z
dc.date.issued2019-07-05
dc.identifier.urihttp://hdl.handle.net/10481/56398
dc.description.abstractIn this paper we extract the aerosol microphysical properties for a collection of mineral dust cases measured by multi-wavelength depolarization Raman lidar systems located at the National Technical University of Athens (NTUA, Athens, Greece) and the Andalusian Institute for Earth System Research (IISTA-CEAMA, Granada, Spain). The lidar-based retrievals were carried out with the Spheroidal Inversion eXperiments software tool (SphInX) developed at the University of Potsdam (Germany). The software uses regularized inversion of a two-dimensional enhancement of the Mie model based on the spheroid-particle approximation with the aspect ratio determining the particle shape. The selection of the cases was based on the transport time from the source regions to the measuring sites. The aerosol optical depth as measured by AERONET ranged from 0.27 to 0.54 (at 500 nm) depending on the intensity of each event. Our analysis showed the hourly mean particle linear depolarization ratio and particle lidar ratio values at 532 nm ranging from 11 to 34% and from 42 to 79 sr respectively, depending on the mixing status, the corresponding air mass pathways and their transport time. Cases with shorter transport time showed good agreement in terms of the optical and SphInX-retrieved microphysical properties between Athens and Granada providing a complex refractive index value equal to 1.4 + 0.004i. On the other hand, the results for cases with higher transport time deviated from the aforementioned ones as well as from each other, providing, in particular, an imaginary part of the refractive index ranging from 0.002 to 0.005. Reconstructions of two-dimensional shape-size distributions for each selected layer showed that the dominant effective particle shape was prolate with diverse spherical contributions. The retrieved volume concentrations reflect overall the intensity of the episodes.es_ES
dc.description.sponsorshipSpanish Ministry of Sciences, Innovation and Universities through project CGL2016-81092,es_ES
dc.description.sponsorshipSpanish Ministry of Education, Culture and Sports through grant FPU14/03684es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.relationThe financial support for EARLINET in the ACTRIS Research Infrastructure Project by the European Union’s Horizon 2020 research and innovation program under grant agreement no. 654169es_ES
dc.subjectmicrophysical propertieses_ES
dc.subjectAerosoles_ES
dc.subjectMineral dustes_ES
dc.titleRetrieval of optical and microphysical properties of transported Saharan dust over Athens and Granada based on multi-wavelength Raman lidar measurements: Study of the mixing processeses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doihttps://doi.org/10.1016/j.atmosenv.2019.116824


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