Seasonal variability of the aerosol parameters over Kanpur, an urban site in Indo-Gangetic basin

被引:55
作者
Dey, S
Tripathi, SN
Singh, RP [1 ]
Holben, BN
机构
[1] Indian Inst Technol, Dept Civil Engn, Kanpur 208016, Uttar Pradesh, India
[2] George Mason Univ, GEOSR, Fairfax, VA 22031 USA
[3] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
来源
ATMOSPHERIC REMOTE SENSING: EARTH'S SURFACE, TROPOSPHERE, STRATOSPHERE AND MESOSPHERE - I | 2005年 / 36卷 / 05期
关键词
aerosols; Indo-Gangetic basin; dust; remote sensing; CIMEL;
D O I
10.1016/j.asr.2005.06.040
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
With the growing antropogenic activities and urbanization, pollution level is found to be increasing in the Indo-Gangetic (IG) basin. This trend of increasing pollution has direct impact on the climatic conditions, especially the increase of haze, fog and cloudy conditions in the region. A ground-based CIMEL radiometer has been deployed on the campus of the Indian Institute of Technology (IIT) Kanpur, India, as a part of the Aerosol Robotic Network (AERONET) program with an objective to characterize the aerosols in the IG basin. The optical properties of the aerosols over Kanpur, which is one of the largest industrial cities in the IG basin, show strong seasonal and inter-annual variations. The fine mode urban/industrial aerosols contribute more than 75% to the observed aerosol optical depth (AOD) during the post-monsoon and winter seasons, whereas the natural dusts contribute similar to 60% to the AOD during the pre-monsoon and monsoon seasons. Effective radius (R-eff) and volume weighted mean radius (R-V), the two best representative parameter of the coarse and fine modes of aerosol size distribution show maximum values during winter season. The increase in the RV is attributed to the hygroscopic growth of fine mode particles in presence of high relative humidity and favorable temperature condition; but the increase in r(eff) is due to the association of the fine mode absorbing particles to the coarser dusts. This is also reflected in low values (< 0.8) of single scattering albedo (SSA) at coarse mode during the season. Higher values of SSA at fine mode indicate dominance of water-soluble aerosols scattering in nature. The linear regression equations between AOD (at 0.67 mu m wavelength) and extinction coefficient due to fine and coarse modes also reveal the relative contribution of the fine and coarse mode particles to the observed optical properties during different seasons in Kanpur. (c) 2005 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:778 / 782
页数:5
相关论文
共 21 条
  • [1] [Anonymous], 0399 ISROGBP
  • [2] Can the state of mixing of black carbon aerosols explain the mystery of 'excess' atmospheric absorption?
    Chandra, S
    Satheesh, SK
    Srinivasan, J
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (19) : L191091 - 4
  • [3] Regional distribution of absorbing efficiency of dust aerosols over India and adjacent continents inferred using satellite remote sensing
    Deepshikha, S
    Satheesh, SK
    Srinivasan, J
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (03) : 1 - 4
  • [4] Derimian Y., 2004, OPT PURA APLIC, V37, P3167
  • [5] Influence of dust storms on the aerosol optical properties over the Indo-Gangetic basin
    Dey, S
    Tripathi, SN
    Singh, RP
    Holben, BN
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D20) : D202111 - 13
  • [6] Analysis of Multi-angle Imaging SpectroRadiometer (MISR) aerosol optical depths over greater India during winter 2001-2004
    Di Girolamo, L
    Bond, TC
    Bramer, D
    Diner, DJ
    Fettinger, F
    Kahn, RA
    Martonchik, JV
    Ramana, MV
    Ramanathan, V
    Rasch, PJ
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (23) : 1 - 5
  • [7] DUBOIS D, 1991, J APPL NONCLASSICAL, V1, P105
  • [8] A flexible inversion algorithm for retrieval of aerosol optical properties from Sun and sky radiance measurements
    Dubovik, O
    King, MD
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D16) : 20673 - 20696
  • [9] Dubovik O, 2002, J ATMOS SCI, V59, P590, DOI 10.1175/1520-0469(2002)059<0590:VOAAOP>2.0.CO
  • [10] 2