Aerosol optical properties of Western Mediterranean basin from multi-year AERONET data

被引:22
|
作者
Benkhalifa, Jamel [1 ]
Leon, Jean Francois [2 ]
Chaabane, Mabrouk [1 ]
机构
[1] FSS, BP 1171, Sfax 3000, Tunisia
[2] Univ Paul Sabatier, CNRS, Lab Aerol, Toulouse, France
关键词
AERONET; Dust aerosol; Aerosol extinction optical depth; Coarse mode; Size distribution; Single scattering albedo; SCATTERING PROPERTIES; SOUTHEASTERN SPAIN; DUST EVENTS; VARIABILITY; TRANSPORT; LAMPEDUSA; RETRIEVAL; SUN; EMISSIONS; SPHEROIDS;
D O I
10.1016/j.jastp.2017.08.029
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Aerosol optical properties including the total and coarse mode aerosol extinction optical depth (AOD(t) and AOD(C) respectively), Angstrom exponent (AE), size distribution, single scattering albedo (SSA) were examined using long-term ground-based radiometric measurements at 9 sites in the Western Mediterranean: Oujda, Malaga, Barcelona, Carpentras, Rome Tor Vergata, Ersa, Ispra, Venice and Evora, during the 4-year study period (2010-2013). The South-North gradient in the fraction of AODC represents the signature of the increasing influence of coarse particles on the optical properties at southern stations. This fraction has a daily mean ranging from 48 +/- 18% at the southern site Oujda and to 8 +/- 8% at Ispra. The low average AE(44-870)value (<0.7) at Oujda confirms the major influence of large dust particles. Conversely, the AOD at urban stations are dominated by fine mode particles. The Angstrom Exponent (AE(444-870)) above 1.5 in Ispra and Venice indicates an atmospheric situation corresponding to the urban pollution controlled by small particles. We have analyzed the intrinsic dust optical properties by selecting the dusty days corresponding to a total optical depth above 0.3 and a fraction of the coarse mode optical depth above 30%. For these cases, the mean A0Dt during dusty days was shown to be close to 0.4. During dusty days, the coarse mode fraction represents 88% of the total volume at Oudja and above 83% for all other sites. There is a weak variability in the mean coarse mode volume median radius, showing an average of 1.98 +/- 0.1. A maximum in the AODC was observed in the summer of 2012, with particular high events on June 27. The forward trajectory starting at Evora on June 27 clearly indicates that all the sites were affected by such dust events in the following days.
引用
收藏
页码:222 / 228
页数:7
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