Aerosol climatology and discrimination of different types over Athens, Greece, based on MODIS data

被引:80
作者
Kaskaoutis, D. G.
Kosmopoulos, P.
Kambezidis, H. D.
Nastos, P. T.
机构
[1] Natl Observ Athens, Inst Environm Res & Sustainable Dev, Atmospher Res Team, GR-11810 Athens, Greece
[2] Univ Ioannina, Dept Phys, Lab Meteorol, GR-45110 Ioannina, Greece
[3] Univ Athens, Dept Geol & Geoenvironm, GR-15784 Athens, Greece
关键词
aerosol optical depth; fine-mode fraction; MODIS; aerosol types; Athens; Greece;
D O I
10.1016/j.atmosenv.2007.05.017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A long-term (2000-2005) monitoring of aerosol data from the moderate resolution imaging spectroradiometer (MODIS) is analyzed focusing on the Greater Athens Area (GAA) in the Eastern Mediterranean region. The MODIS aerosol optical depth standard product (AOD at 550 nm) and its respective ratio attributed to fine-mode (FM) particles are employed to evaluate the seasonal variability of the aerosol properties over Athens. The climatological trend of both parameters in the period 2000-2005 is nearly absent, while remarkable year-to-year variability can be observed. The seasonal analysis reveals a significant AOD variability over Athens, with minimum values in winter (AOD(550) similar to 0.2), and maximum in summer (AOD(550)similar to 0.45). Regarding the FM fraction, maximum values are present in spring and minimum in summer, thus revealing the dominance of FM and coarse-mode particles, respectively. For the whole data set, a method is implemented to distinguish the main aerosol types (urban/industrial (hereafter UI), clean maritime (hereafter CM type) and desert dust (hereafter DD) over Athens, based on both AOD and FM values. Because of the mixing processes in the atmosphere the majority of the cases (46.6%) belong to a mixed (hereafter MT) aerosol type. The U aerosols are more frequent in spring (41.2%) and less in winter (9.1 %), while the coarse particles, probably DD, more frequent in summer (35.8%) and less in winter (3.5%). In contrast, the clean atmospheric conditions are more frequent in winter (23.9%), when the mixing processes are also well established (63.5%). For each aerosol type, the mean AOD(550) and FM values are also computed. Their seasonal variability exhibits a clear summer maximum for UI, CM and MT aerosols, while the DD exhibits maximum in spring. As regards the FM values of the different aerosol types they exhibit a rather constant variation with small fluctuations from season to season. (c) 2007 Elsevier Ltd. All rights reserved.
引用
收藏
页码:7315 / 7329
页数:15
相关论文
共 40 条
[1]  
Adamopoulos AD, 2000, FRESEN ENVIRON BULL, V9, P201
[2]  
AMIRIDIS V, 2005, J GEOPHYSICAL RES, V110
[3]  
[Anonymous], [No title captured]
[4]   Recent increase of Saharan dust transport over the Mediterranean Sea, as revealed from ocean color satellite (SeaWiFS) observations [J].
Antoine, D. ;
Nobileau, D. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D12)
[5]   Raman lidar and sunphotometric measurements of aerosol optical properties over Thessaloniki, Greece during a biomass burning episode [J].
Balis, DS ;
Amiridis, V ;
Zerefos, C ;
Gerasopoulos, E ;
Andreae, M ;
Zanis, P ;
Kazantzidis, A ;
Kazadzis, S ;
Papayannis, A .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (32) :4529-4538
[6]   Aerosol seasonal variability over the Mediterranean region and relative impact of maritime, continental and Saharan dust particles over the basin from MODIS data in the year 2001 [J].
Barnaba, F ;
Gobbi, GP .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2004, 4 :2367-2391
[7]  
CHIN M, 2004, J GEOPHYSICAL RES, V109
[8]   Global monitoring of air pollution over land from the Earth Observing System-Terra Moderate Resolution Imaging Spectroradiometer (MODIS) [J].
Chu, DA ;
Kaufman, YJ ;
Zibordi, G ;
Chern, JD ;
Mao, J ;
Li, CC ;
Holben, BN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D21)
[9]  
CHU DA, 2002, GEOPHYSICAL RES LETT, V29
[10]   ASSESSMENT OF THE AFRICAN AIRBORNE DUST MASS OVER THE WESTERN MEDITERRANEAN-SEA USING METEOSAT DATA [J].
DULAC, F ;
TANRE, D ;
BERGAMETTI, G ;
BUATMENARD, P ;
DESBOIS, M ;
SUTTON, D .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D2) :2489-2506