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 (lid...

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Main Authors: A. Nisantzi, R. E. Mamouri, A. Ansmann, G. L. Schuster, D. G. Hadjimitsis
Format: Article
Language:English
Published: Copernicus Publications 2015-06-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/7071/2015/acp-15-7071-2015.pdf
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author A. Nisantzi
R. E. Mamouri
A. Ansmann
G. L. Schuster
D. G. Hadjimitsis
author_facet A. Nisantzi
R. E. Mamouri
A. Ansmann
G. L. Schuster
D. G. Hadjimitsis
author_sort A. Nisantzi
collection DOAJ
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.
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spelling doaj.art-681a7c066df341d4b406ac680cb126812022-12-22T02:15:55ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-06-0115127071708410.5194/acp-15-7071-2015Middle East versus Saharan dust extinction-to-backscatter ratiosA. Nisantzi0R. E. Mamouri1A. Ansmann2G. L. Schuster3D. G. Hadjimitsis4Cyprus University of Technology, Dep. of Civil Engineering and Geomatics, Limassol, CyprusCyprus University of Technology, Dep. of Civil Engineering and Geomatics, Limassol, CyprusLeibniz Institute for Tropospheric Research, Leipzig, GermanyNASA Langley Research Center, Hampton, Virginia, USACyprus University of Technology, Dep. of Civil Engineering and Geomatics, Limassol, CyprusFour 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.http://www.atmos-chem-phys.net/15/7071/2015/acp-15-7071-2015.pdf
spellingShingle A. Nisantzi
R. E. Mamouri
A. Ansmann
G. L. Schuster
D. G. Hadjimitsis
Middle East versus Saharan dust extinction-to-backscatter ratios
Atmospheric Chemistry and Physics
title 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_short Middle East versus Saharan dust extinction-to-backscatter ratios
title_sort middle east versus saharan dust extinction to backscatter ratios
url http://www.atmos-chem-phys.net/15/7071/2015/acp-15-7071-2015.pdf
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