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...
Main Authors: | , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
München : European Geopyhsical Union
2015
|
Subjects: | |
Online Access: | https://doi.org/10.34657/1098 https://oa.tib.eu/renate/handle/123456789/316 |
id |
ftleibnizopen:oai:oai.leibnizopen.de:Kd-Pm4YBdbrxVwz6_IfD |
---|---|
record_format |
openpolar |
spelling |
ftleibnizopen:oai:oai.leibnizopen.de:Kd-Pm4YBdbrxVwz6_IfD 2023-05-15T13:06:13+02:00 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://doi.org/10.34657/1098 https://oa.tib.eu/renate/handle/123456789/316 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ CC-BY Atmospheric Chemistry and Physics, Volume 15, Issue 12, Page 7071-7084 550 article Text 2015 ftleibnizopen https://doi.org/10.34657/1098 2023-03-01T07:30:51Z 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. publishedVersion Article in Journal/Newspaper Aerosol Robotic Network LeibnizOpen (The Leibniz Association) |
institution |
Open Polar |
collection |
LeibnizOpen (The Leibniz Association) |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
550 |
spellingShingle |
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 |
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. publishedVersion |
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://doi.org/10.34657/1098 https://oa.tib.eu/renate/handle/123456789/316 |
genre |
Aerosol Robotic Network |
genre_facet |
Aerosol Robotic Network |
op_source |
Atmospheric Chemistry and Physics, Volume 15, Issue 12, Page 7071-7084 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.34657/1098 |
_version_ |
1765996864547586048 |