Monitoring spatio-temporal aerosol patterns over Pakistan based on MODIS, TOMS and MISR satellite data and a HYSPLIT model

被引:141
|
作者
Alam, Khan [1 ]
Qureshi, Salman [1 ,2 ]
Blaschke, Thomas [1 ]
机构
[1] Salzburg Univ, Dept Geog & Geol, A-5020 Salzburg, Austria
[2] Univ Karachi, Dept Geog, Karachi 75270, Pakistan
关键词
Aerosols; TOMS; MODIS; MISR; AERONET; HYSPLIT; AOD; Remote sensing; Pakistan; BLACK CARBON AEROSOLS; INDO-GANGETIC BASIN; OPTICAL DEPTH; ABSORBING AEROSOLS; SAHARAN DUST; AERONET; CLIMATE; VARIABILITY; CLOUD; THICKNESS;
D O I
10.1016/j.atmosenv.2011.05.055
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Three different satellite-borne sensors, namely the Total Ozone Mapping Spectrometer (TOMS), the Moderate Resolution Imaging Spectroradiometer (MODIS), and the Multi-angle Imaging Spectroradiometer (MISR), were used to investigate the spatial and temporal variations of aerosols over several cities in Pakistan. A Hybrid Single Particle Lagrangian Integrated Trajectory (HYSPLIT) model was used for trajectory analysis in order to reconstruct the origins of air masses and understand the spatio-temporal variability of aerosol concentrations. Recent MODIS aerosol data (2002-2008) and earlier TOMS data (1979-2001) revealed increasing concentrations of aerosols over Pakistan and adjacent areas. Validation of MODIS and MISR derived aerosol optical depths (AODs) with Aerosol Robotic Network (AERONET) data for 2007 demonstrated that the MISR data was more accurate when close to the ocean, while the MODIS was more accurate over vegetated areas. The relationship between MODIS and MISR AOD data from 2002 to 2008 was analyzed, revealing a strong correlation between the two datasets. An assessment of seasonal variability in AOD for industrial, urban, semi-urban, rural, and semi-arid areas revealed maximum AOD values during the summer over all the areas investigated. Back trajectory analyses indicated that while winter air masses reaching Pakistan had travelled long distances, summer air masses had travelled only short distances. The higher aerosol concentrations during the summer are interpreted to be a result of the air masses spending more time over land during the summer than they do during the winter. While monsoonal rainfall tends to reduce aerosol concentrations by washing aerosols out of the atmosphere, this effect is mainly restricted to the eastern and south-eastern parts of Pakistan. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:4641 / 4651
页数:11
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