Wintertime characteristics of aerosols at middle Indo-Gangetic Plain: Impacts of regional meteorology and long range transport

被引:68
|
作者
Kumar, M. [1 ]
Tiwari, S. [2 ]
Murari, V. [1 ]
Singh, A. K. [2 ]
Banerjee, T. [1 ]
机构
[1] Banaras Hindu Univ, Inst Environm & Sustainable Dev, Varanasi 221005, Uttar Pradesh, India
[2] Banaras Hindu Univ, Dept Phys, Atmospher Res Lab, Varanasi 221005, Uttar Pradesh, India
关键词
Aerosol; Aerosol optical depth; CALIPSO; Indo-Gangetic Plain; MODIS; Trans-boundary; PARTICULATE MATTER; AIR-POLLUTION; OPTICAL DEPTH; MASS CONCENTRATIONS; MODIS; DELHI; FINE; PARAMETERS; RETRIEVAL; QUALITY;
D O I
10.1016/j.atmosenv.2015.01.014
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To develop a coherent picture of possible origin of Asian aerosol, transport and meteorological interaction; wintertime aerosol (January, 1 to March, 31, 2014 (n = 90)) were measured in middle IGP in terms of aerosol Mass loading, optical properties, attitudinal distributions and both high and low altitude transportation. Both space-borne passive (Aqua and Terra MODIS) and active sensor (CALIPSO-CALIOP) based measurements were concurrently used over the selected transect (25 degrees 10'-25 degrees 19'N and 82 degrees 54' -83 4'E). Exceptionally high aerosol mass loading was recorded for PM10 (233 +/- 58.37 mu g m(-3)) and PM2.5 (138 +/- 47.12 mu g m(-3)). Daily variations of PM2.5/PM10 persist in a range of 0.25-0.97 (mean = 0.60 +/- 0.14; n = 90) and were in accordance to computed Angstrom exponent (0.078-1.407; mean: 1.002 +/- 0.254) explaining concurrent contribution of both PM2.5 and PM10 for the region. Space borne (Aqua MODIS-AOD: 0.259-2.194) and ground based (MTP-AOD: 0.066-1.239) AODs revealed significant temporal variability and moderate association in terms of PM10 (MODIS-AOD: 0.46; MTP-AOD: 0.56) and PM2.5 (MODIS-AOD: 0.54; MTP-AOD: 0.39). Varying association of AOD and aerosol mass loading was also explained in terms of meteorological variables. CALIPSO altitude-orbit-cross-section profiles revealed presence of non-spherical coarse particulates (altitude: 1.2-5.4 km) and dominance of spherical fine particulates (altitude: 0.1-4.2 km). Contribution of trans-boundary aerosols transportation to mass loadings at middle IGP were recognized through lagrangian particle dispersion model, synoptic vector wind profiles at different geopotential heights and satellite images. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:162 / 175
页数:14
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