Two years of free-tropospheric aerosol layers observed over Portugal by lidar

被引:37
作者
Preissler, J. [1 ]
Wagner, F. [1 ]
Guerrero-Rascado, J. L. [1 ,2 ,3 ]
Silva, A. M. [1 ]
机构
[1] Univ Evora, Evora Geophys Ctr, Evora, Portugal
[2] Univ Granada Autonomous Govt Andalusia, Andalusian Ctr Environm Res CEAMA, Granada, Spain
[3] Univ Granada, Dept Appl Phys, Granada, Spain
关键词
atmospheric remote sensing; lidar; free tropospheric aerosol; aerosol characterization; EUROPEAN POLLUTION OUTBREAKS; MICROPHYSICAL PARTICLE PROPERTIES; SPECTRAL-RESOLUTION LIDAR; RAMAN LIDAR; OPTICAL-PROPERTIES; SAHARAN DUST; MULTIWAVELENGTH LIDAR; IBERIAN PENINSULA; ASIAN DUST; BACKSCATTER;
D O I
10.1002/jgrd.50350
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Multi-wavelength Raman light detection and ranging (lidar) observations were analyzed, which were performed in Evora, Portugal, during more than 2years on a regular basis in the framework of the European Aerosol Research Lidar Network (EARLINET). An aerosol characterization in terms of the lidar ratios at 355 and 532nm and the extinction and backscatter related angstrom ngstrom exponents is presented. Aerosol layers in the free troposphere were classified according to their origin. Clear differences in the intensive optical properties were found for layers of mineral dust from the Sahara and from Asia, of anthropogenic aerosol from Europe and from North America, as well as of biomass burning smoke from the Iberian Peninsula and from North America, respectively. In general, the mean angstrom ngstrom exponents of aerosol layers of the same type, but from closer source regions, were smaller than those from aerosol layers transported over a longer distance. This hints at the deposition of large particles along the transportation path, especially for anthropogenic aerosol and mineral dust. Besides, the seasonal behavior of aerosol in the free troposphere over Evora was studied. Seventy-three percent of the detected layers were observed during spring and summer. On average, the layers were highest in summer with an overall mean layer height of (3.8 +/- 1.9)km above sea level (asl), and lowest in winter with (2.3 +/- 0.9)kmasl.
引用
收藏
页码:3676 / 3686
页数:11
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