Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations
Four years (2014-2017) of observations of depolarization Raman Lidar systems of four EARLINET (European Aerosol research Lidar Network) stations [from West to East: Granada (Spain), Potenza (Italy), Athens (Greece) and Limassol (Cyprus)] were collected and used to a statistical analysis of Saharan d...
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doaj-eda7411b440c4efb99abfdf5935ddc8c2021-08-02T13:30:44ZengEDP SciencesEPJ Web of Conferences2100-014X2020-01-012370501010.1051/epjconf/202023705010epjconf_ilrc292020_05010Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet StationsSoupiona Ourania0Papayannis Alex1Mylonaki Maria2Papagiannopoulos Nikolaos3Ortiz-Amezcua PabloMamouri Rodanthi E.4Groß Silke5Papanikolaou Christina A.6Kokkalis Panagiotis7Applied Mathematics and Physical Sciences, National Technical University of AthensApplied Mathematics and Physical Sciences, National Technical University of AthensApplied Mathematics and Physical Sciences, National Technical University of AthensConsiglio Nazionale delle Ricerche, Istituto di Metodologie per l’Analisi AmbientaleDepartment of Civil Engineering and Geomatics, ERATOSTHENES Research Centre, Cyprus University of TechnologyInstitute of Atmospheric Physics, Deutsches Zentrum für Luft- und Raumfahrt (DLR)Applied Mathematics and Physical Sciences, National Technical University of AthensDepartment of Physics, Kuwait UniversityFour years (2014-2017) of observations of depolarization Raman Lidar systems of four EARLINET (European Aerosol research Lidar Network) stations [from West to East: Granada (Spain), Potenza (Italy), Athens (Greece) and Limassol (Cyprus)] were collected and used to a statistical analysis of Saharan dust events over Mediterranean basin. In this study, emphasis is given to the consistency of the particle linear depolarization ratio (δp532), the extinction-to-backscatter ratio mentioned as Lidar Ratio (LR532) and the Aerosol Optical Thickness (AOT532) within the observed Saharan dust layers, corresponding to the visible range (532 nm). Geometrical properties and clusters of aerosol mixtures are also presented. Our clustering was based on previous classification by airborne High Spectral Resolution Lidar (HSRL) observations and was further supported by backward trajectory analysis. We found mean δp532 values of 0.24±0.05, 0.26±0.06, 0.28±0.05 and 0.28±0.04, mean LR532 values of 52±8 sr, 51±9 sr, 52±9 sr and 49±6 sr, mean AOT532 values of 0.40±0.31, 0.11±0.07, 0.12±0.10 and 0.32±0.17 and mean layer thicknesses of 3392±1458 m, 2150±1082 m, 1872±816 m and 1716±567 m for Granada, Potenza, Athens and Limassol respectively. This work could assist in bridging the existing gaps related to the extensive and intensive dust aerosol properties over the Mediterranean and enriching the bibliography about mixed aerosol layers from different sources (e.g. dust and biomass burning (BB) aerosols, dust and urban/ industrial aerosols).https://www.epj-conferences.org/articles/epjconf/pdf/2020/13/epjconf_ilrc292020_05010.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Soupiona Ourania Papayannis Alex Mylonaki Maria Papagiannopoulos Nikolaos Ortiz-Amezcua Pablo Mamouri Rodanthi E. Groß Silke Papanikolaou Christina A. Kokkalis Panagiotis |
spellingShingle |
Soupiona Ourania Papayannis Alex Mylonaki Maria Papagiannopoulos Nikolaos Ortiz-Amezcua Pablo Mamouri Rodanthi E. Groß Silke Papanikolaou Christina A. Kokkalis Panagiotis Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations EPJ Web of Conferences |
author_facet |
Soupiona Ourania Papayannis Alex Mylonaki Maria Papagiannopoulos Nikolaos Ortiz-Amezcua Pablo Mamouri Rodanthi E. Groß Silke Papanikolaou Christina A. Kokkalis Panagiotis |
author_sort |
Soupiona Ourania |
title |
Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations |
title_short |
Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations |
title_full |
Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations |
title_fullStr |
Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations |
title_full_unstemmed |
Saharan Dust Events Over the Northern Mediterranean: 4 Years of Measurements Over 4 Earlinet Stations |
title_sort |
saharan dust events over the northern mediterranean: 4 years of measurements over 4 earlinet stations |
publisher |
EDP Sciences |
series |
EPJ Web of Conferences |
issn |
2100-014X |
publishDate |
2020-01-01 |
description |
Four years (2014-2017) of observations of depolarization Raman Lidar systems of four EARLINET (European Aerosol research Lidar Network) stations [from West to East: Granada (Spain), Potenza (Italy), Athens (Greece) and Limassol (Cyprus)] were collected and used to a statistical analysis of Saharan dust events over Mediterranean basin.
In this study, emphasis is given to the consistency of the particle linear depolarization ratio (δp532), the extinction-to-backscatter ratio mentioned as Lidar Ratio (LR532) and the Aerosol Optical Thickness (AOT532) within the observed Saharan dust layers, corresponding to the visible range (532 nm). Geometrical properties and clusters of aerosol mixtures are also presented. Our clustering was based on previous classification by airborne High Spectral Resolution Lidar (HSRL) observations and was further supported by backward trajectory analysis. We found mean δp532 values of 0.24±0.05, 0.26±0.06, 0.28±0.05 and 0.28±0.04, mean LR532 values of 52±8 sr, 51±9 sr, 52±9 sr and 49±6 sr, mean AOT532 values of 0.40±0.31, 0.11±0.07, 0.12±0.10 and 0.32±0.17 and mean layer thicknesses of 3392±1458 m, 2150±1082 m, 1872±816 m and 1716±567 m for Granada, Potenza, Athens and Limassol respectively.
This work could assist in bridging the existing gaps related to the extensive and intensive dust aerosol properties over the Mediterranean and enriching the bibliography about mixed aerosol layers from different sources (e.g. dust and biomass burning (BB) aerosols, dust and urban/ industrial aerosols). |
url |
https://www.epj-conferences.org/articles/epjconf/pdf/2020/13/epjconf_ilrc292020_05010.pdf |
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