Issue |
EPJ Web of Conferences
Volume 119, 2016
The 27th International Laser Radar Conference (ILRC 27)
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Article Number | 23016 | |
Number of page(s) | 4 | |
Section | Poster Session (Aerosol Observations and Retrievals II) | |
DOI | https://doi.org/10.1051/epjconf/201611923016 | |
Published online | 07 June 2016 |
https://doi.org/10.1051/epjconf/201611923016
Tropospheric Vertical Profiles of Aerosol Optical, Microphysical and Concentration Properties in the Frame of the Hygra-CD Campaign (Athens, Greece 2014): A Case Study of Long-Range Transport of Mixed Aerosols
1 Laser Remote Sensing Laboratory, National Technical University of Athens, 15780 Athens, Greece
2 University of Hertfordshire, Hatfield, Hertfordshire, AL10 9AB, UK
3 INOE, National R&D Institute for Optoelectronics, Magurele, Romania
4 Physikalisch-Meteorologisches Observatorium Davos, World Radiation Center, Switzerland
5 IAASARS, National Observatory of Athens, Greece
* Email: apdlidar@central.ntua.gr
Published online: 7 June 2016
Combined multi-wavelength aerosol Raman lidar and sun photometry measurements were performed during the HYGRA-CD campaign over Athens, Greece during May-June 2014. The retrieved aerosol optical properties (3 aerosol backscatter at 355-532-1064 nm and 2 aerosol extinction profiles at 355-532 nm) were used as input to an inversion code to retrieve the aerosol microphysical properties (effective radius reff and number concentration N) using regularization techniques. Additionally, the volume concentration profile was derived for fine particles using the LIRIC code. In this paper we selected a complex case study of long-range transport of mixed aerosols (biomass burning particles mixed with dust) arriving over Athens between 10-12 June 2014 in the 1.5-4 km height. Between 2-3 km height we measured mean lidar ratios (LR) ranging from 45 to 58 sr (at 355 and 532 nm), while the Ångström exponent (AE) aerosol extinction-related values (355nm/532nm) ranged between 0.8-1.3. The retrieved values of reff and N ranged from 0.19±0.07 to 0.22±0.07 μm and 460±230 to 2200±2800 cm-3, respectively. The aerosol linear depolarization ratio (δ) at 532 nm was lower than 5-7% (except for the Saharan dust cases, where δ~10-15%).
© Owned by the authors, published by EDP Sciences, 2016
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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