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| Hauptseite > Workflowsammlungen > Öffentliche Einträge > Comparison of vertical aerosol extinction coefficients from in-situ and LIDAR measurements > print |
| Hauptseite > Workflowsammlungen > Öffentliche Einträge > Comparison of vertical aerosol extinction coefficients from in-situ and LIDAR measurements > print |
| 001 | 278668 | ||
| 005 | 20240712100948.0 | ||
| 024 | 7 | _ | |a 10.5194/acpd-15-18609-2015 |2 doi |
| 024 | 7 | _ | |a 1680-7367 |2 ISSN |
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| 037 | _ | _ | |a FZJ-2015-06993 |
| 082 | _ | _ | |a 550 |
| 100 | 1 | _ | |a Rosati, B. |0 P:(DE-HGF)0 |b 0 |
| 245 | _ | _ | |a Comparison of vertical aerosol extinction coefficients from in-situ and LIDAR measurements |
| 260 | _ | _ | |a Katlenburg-Lindau |c 2015 |b EGU |
| 336 | 7 | _ | |a Journal Article |b journal |m journal |0 PUB:(DE-HGF)16 |s 1449123551_16686 |2 PUB:(DE-HGF) |
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| 336 | 7 | _ | |a article |2 DRIVER |
| 520 | _ | _ | |a Vertical profiles of aerosol optical properties were explored in a case study near the San Pietro Capofiume (SPC) ground station during the PEGASOS Po Valley campaign in the summer of 2012. A Zeppelin NT airship was employed to investigate the effect of the dynamics of the planetary boundary layer at altitudes between ~ 50–800 m above ground. Determined properties included the aerosol size distribution, the hygroscopic growth factor, the effective index of refraction and the light absorption coefficient. The first three parameters were used to retrieve the light scattering coefficient. Simultaneously, direct measurements of both the scattering and absorption coefficient were carried out at the SPC ground station. Additionally, a LIDAR system provided aerosol extinction coefficients for a vertically resolved comparison between in-situ and remote sensing results. First, the airborne results at low altitudes were validated with the ground measurements. Agreement within approximately ±25 and ±20% was found for the dry scattering and absorption coefficient, respectively. The single scattering albedo, ranged between 0.83 to 0.95, indicating the importance of the absorbing particles in the Po Valley region. A clear layering of the atmosphere was observed during the beginning of the flight (until ~ 10 local time) before the mixed layer (ML) was fully developed. Highest extinction coefficients were found at low altitudes, in the new ML, while values in the residual layer, which could be probed at the beginning of the flight at elevated altitudes, were lower. At the end of the flight (after ~ 12 local time) the ML was fully developed, resulting in constant extinction coefficients at all altitudes measured on the Zeppelin NT. LIDAR results captured these dynamic features well and good agreement was found for the extinction coefficients compared to the in-situ results, using fixed LIDAR ratios (LR) between 30 and 70 sr for the altitudes probed with the Zeppelin. These LR are consistent with values for continental aerosol particles that can be expected in this region. |
| 536 | _ | _ | |a 243 - Tropospheric trace substances and their transformation processes (POF3-243) |0 G:(DE-HGF)POF3-243 |c POF3-243 |f POF III |x 0 |
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| 700 | 1 | _ | |a Herrmann, E. |0 P:(DE-HGF)0 |b 1 |e Corresponding author |
| 700 | 1 | _ | |a Bucci, S. |0 P:(DE-HGF)0 |b 2 |
| 700 | 1 | _ | |a Fierli, F. |0 P:(DE-HGF)0 |b 3 |
| 700 | 1 | _ | |a Cairo, F. |0 P:(DE-HGF)0 |b 4 |
| 700 | 1 | _ | |a Gysel, M. |0 P:(DE-HGF)0 |b 5 |
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| 700 | 1 | _ | |a Größ, J. |0 P:(DE-HGF)0 |b 7 |
| 700 | 1 | _ | |a Gobbi, G. P. |0 P:(DE-HGF)0 |b 8 |
| 700 | 1 | _ | |a Di Liberto, L. |0 P:(DE-HGF)0 |b 9 |
| 700 | 1 | _ | |a Di Donfrancesco, G. |0 P:(DE-HGF)0 |b 10 |
| 700 | 1 | _ | |a Wiedensohler, A. |0 P:(DE-HGF)0 |b 11 |
| 700 | 1 | _ | |a Weingartner, E. |0 P:(DE-HGF)0 |b 12 |
| 700 | 1 | _ | |a Virtanen, A. |0 P:(DE-HGF)0 |b 13 |
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| 700 | 1 | _ | |a Baltensperger, U. |0 P:(DE-HGF)0 |b 15 |
| 773 | _ | _ | |a 10.5194/acpd-15-18609-2015 |g Vol. 15, no. 13, p. 18609 - 18651 |0 PERI:(DE-600)2069857-4 |n 13 |p 18609 - 18651 |t Atmospheric chemistry and physics / Discussions |v 15 |y 2015 |x 1680-7375 |
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