Middle East versus Saharan dust extinction-to-backscatter ratios

Four years (2010–2013) of observations with polarization lidar and sun/sky photometer at the combined European Aerosol Research Lidar Network (EARLINET) and Aerosol Robotic Network (AERONET) site of Limassol (34.7° N, 33° E), Cyprus, were used to compare extinction-to-backscatter ratios (lidar ratio...

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Main Authors: Nisantzi, A., Mamouri, R.E., Ansmann, A., Schuster, G.L., Hadjimitsis, D.G.
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2015
Subjects:
Online Access:https://oa.tib.eu/renate/handle/123456789/316
https://doi.org/10.34657/1098
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spelling fttibhannoverren:oai:oa.tib.eu:123456789/316 2024-09-15T17:35:12+00:00 Middle East versus Saharan dust extinction-to-backscatter ratios Nisantzi, A. Mamouri, R.E. Ansmann, A. Schuster, G.L. Hadjimitsis, D.G. 2015 application/pdf https://oa.tib.eu/renate/handle/123456789/316 https://doi.org/10.34657/1098 eng eng München : European Geopyhsical Union DOI:https://doi.org/10.5194/acp-15-7071-2015 https://doi.org/10.34657/1098 https://oa.tib.eu/renate/handle/123456789/316 CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ frei zugänglich ddc:550 status-type:publishedVersion doc-type:Article doc-type:Text 2015 fttibhannoverren https://doi.org/10.34657/109810.5194/acp-15-7071-2015 2024-06-26T23:32:42Z Four years (2010–2013) of observations with polarization lidar and sun/sky photometer at the combined European Aerosol Research Lidar Network (EARLINET) and Aerosol Robotic Network (AERONET) site of Limassol (34.7° N, 33° E), Cyprus, were used to compare extinction-to-backscatter ratios (lidar ratios) for desert dust from Middle East deserts and the Sahara. In an earlier article, we analyzed one case only and found comparably low lidar ratios < 40 sr for Middle East dust. The complex data analysis scheme is presented. The quality of the retrieval is checked within a case study by comparing the results with respective Raman lidar solutions for particle backscatter, extinction, and lidar ratio. The applied combined lidar/photometer retrievals corroborate recent findings regarding the difference between Middle East and Saharan dust lidar ratios. We found values from 43–65 sr with a mean (±standard deviation) of 53 ± 6 sr for Saharan dust and from 33–48 sr with a mean of 41 ± 4 sr for Middle East dust for the wavelength of 532 nm. The presented data analysis, however, also demonstrates the difficulties in identifying the optical properties of dust even during outbreak situations in the presence of complex aerosol mixtures of desert dust, marine particles, fire smoke, and anthropogenic haze. Article in Journal/Newspaper Aerosol Robotic Network Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
institution Open Polar
collection Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
op_collection_id fttibhannoverren
language English
topic ddc:550
spellingShingle ddc:550
Nisantzi, A.
Mamouri, R.E.
Ansmann, A.
Schuster, G.L.
Hadjimitsis, D.G.
Middle East versus Saharan dust extinction-to-backscatter ratios
topic_facet ddc:550
description Four years (2010–2013) of observations with polarization lidar and sun/sky photometer at the combined European Aerosol Research Lidar Network (EARLINET) and Aerosol Robotic Network (AERONET) site of Limassol (34.7° N, 33° E), Cyprus, were used to compare extinction-to-backscatter ratios (lidar ratios) for desert dust from Middle East deserts and the Sahara. In an earlier article, we analyzed one case only and found comparably low lidar ratios < 40 sr for Middle East dust. The complex data analysis scheme is presented. The quality of the retrieval is checked within a case study by comparing the results with respective Raman lidar solutions for particle backscatter, extinction, and lidar ratio. The applied combined lidar/photometer retrievals corroborate recent findings regarding the difference between Middle East and Saharan dust lidar ratios. We found values from 43–65 sr with a mean (±standard deviation) of 53 ± 6 sr for Saharan dust and from 33–48 sr with a mean of 41 ± 4 sr for Middle East dust for the wavelength of 532 nm. The presented data analysis, however, also demonstrates the difficulties in identifying the optical properties of dust even during outbreak situations in the presence of complex aerosol mixtures of desert dust, marine particles, fire smoke, and anthropogenic haze.
format Article in Journal/Newspaper
author Nisantzi, A.
Mamouri, R.E.
Ansmann, A.
Schuster, G.L.
Hadjimitsis, D.G.
author_facet Nisantzi, A.
Mamouri, R.E.
Ansmann, A.
Schuster, G.L.
Hadjimitsis, D.G.
author_sort Nisantzi, A.
title Middle East versus Saharan dust extinction-to-backscatter ratios
title_short Middle East versus Saharan dust extinction-to-backscatter ratios
title_full Middle East versus Saharan dust extinction-to-backscatter ratios
title_fullStr Middle East versus Saharan dust extinction-to-backscatter ratios
title_full_unstemmed Middle East versus Saharan dust extinction-to-backscatter ratios
title_sort middle east versus saharan dust extinction-to-backscatter ratios
publisher München : European Geopyhsical Union
publishDate 2015
url https://oa.tib.eu/renate/handle/123456789/316
https://doi.org/10.34657/1098
genre Aerosol Robotic Network
genre_facet Aerosol Robotic Network
op_relation DOI:https://doi.org/10.5194/acp-15-7071-2015
https://doi.org/10.34657/1098
https://oa.tib.eu/renate/handle/123456789/316
op_rights CC BY 3.0 Unported
https://creativecommons.org/licenses/by/3.0/
frei zugänglich
op_doi https://doi.org/10.34657/109810.5194/acp-15-7071-2015
_version_ 1810444490429693952