Investigation of the Atmospheric Boundary Layer and Optical Characteristics of the Atmospheric Aerosols over Sofia in Summer 2016

被引:0
作者
Kolev, Nikolay [1 ,2 ]
Savov, Plamen [1 ]
Evgenieva, Tsvetelina [2 ]
Miloshev, Nikolay [3 ]
Gueorguiev, Orlin [4 ]
Batchvarova, Ekaterina [4 ]
Kolarova, Maria [4 ]
Danchovski, Ventsislav [5 ]
Ivanov, Danko [5 ]
Petkov, Doino [6 ]
机构
[1] Univ Min & Geol St Ivan Rilski, Dept Phys, Sofia, Bulgaria
[2] Bulgarian Acad Sci, Inst Elect, Sofia, Bulgaria
[3] Bulgarian Acad Sci, Natl Inst Geophys Geodesy & Geog, Sofia, Bulgaria
[4] Bulgarian Acad Sci, Natl Inst Meteorol & Hydrol, Sofia, Bulgaria
[5] Sofia Univ St Kliment Ohridsky, Dept Meteorol & Geophys, Fac Phys, Sofia, Bulgaria
[6] Bulgarian Acad Sci, Space Res & Technol Inst, Sofia, Bulgaria
来源
10TH JUBILEE CONFERENCE OF THE BALKAN PHYSICAL UNION | 2019年 / 2075卷
关键词
BULGARIA;
D O I
10.1063/1.5091262
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Observations of the aerosols vertical distribution and an assessment of their optical properties on clear sunny days and days with Saharan dust intrusions were carried out in the summer of 2016 in the mountain valley of Sofia, Bulgaria. In this paper, some of the results obtained during Saharan dust intrusions are presented. Measurements were carried out with active and passive remote sensing devices as well as with in-situ ones. A ceilometer CHM-15k, a sun photometer Microtops II, an ozonometer Microtops II and a laser particle counter (LPC) PC 200 were used. The atmospheric boundary layer (ABL) height was determined from the high temporal and spatial resolution ceilometer data and from aerological sounding. The changes in fine particle concentration in space and time were measured by the sixchannel LPC located in the Borisova Gradina Park, Sofia. HYSPLIT back trajectory model and the BSC-DREAM dust model were used as additional source of information for selected days. The observed ABL height varied from 200 to 2500 in for the presented experimental days. During the campaign, the aerosol optical depth (AOD) at wavelength lambda = 380 nm ranged from 0.30 to 0.56, at lambda= 500nm - from 0.18 to 0.30 and at lambda = 1020 nm - from 0.01 to 0.10. The water vapor content (WVC) changed between 1.5 cm and 2.1 cm. The total ozone content (TOC) varied from 225 DU to 275 DU.
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页数:6
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