2016
DOI: 10.1016/j.atmosenv.2015.07.038
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Aerosol characteristics in north-east India using ARFINET spectral optical depth measurements

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Cited by 50 publications
(46 citation statements)
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“…Significant contribution of absorbing aerosols to lower atmospheric warming over different parts of NE region of India has also been reported by Gogoi et al [62]. Pathak et al [63] have reported that atmospheric forcing due to composite aerosols over Imphal (a valley location south of DMD in NE region of India) was 25. . The global mean clear-sky ARF at the TOA and the surface are however found to be negative [64].…”
Section: Aerosol Radiative Forcingmentioning
confidence: 83%
“…Significant contribution of absorbing aerosols to lower atmospheric warming over different parts of NE region of India has also been reported by Gogoi et al [62]. Pathak et al [63] have reported that atmospheric forcing due to composite aerosols over Imphal (a valley location south of DMD in NE region of India) was 25. . The global mean clear-sky ARF at the TOA and the surface are however found to be negative [64].…”
Section: Aerosol Radiative Forcingmentioning
confidence: 83%
“…[] and Pathak et al . [] have also reported the peaking of columnar AOD in the premonsoon month March from the study of long‐term columnar aerosol optical depth properties over Dibrugarh. This provides a clear indication of possible elevated layers of absorbing aerosols, most probably above the atmospheric boundary layer, during the premonsoon season when the near‐surface BC concentrations are reduced from their peak values in winter.…”
Section: Resultsmentioning
confidence: 99%
“…Locally, the region is rich in its large extent of green tea gardens and forest covers in most of its part and devoid of major anthropogenic and industrial sources. However, the emission of carbonaceous aerosols from the scattered brick kilns and oil wells provide local contribution to the absorbing aerosol concentrations over this region [ Gogoi et al ., ; Pathak et al ., ]. The major emissions from oil and gas exploration are due to the flaring, venting, and purging of gases (including black smoke emissions); combustion of diesel engines; operation of fire protection systems; road traffic; and fugitive gas losses.…”
Section: Introductionmentioning
confidence: 99%
“…They have shown the spatial distinctiveness and the seasonality of aerosol types (anthropogenic, dust and sea-salt) over the different parts of Indian mainland and delineated the importance of long-range transport (especially of mineral dust from the Middle East, eastern Africa and West Asian deserts, and of sea-salt from the Arabian Sea and Indian Ocean). Syntheses at sub-regional scales have established and quantified, to a certain extent, the significant impacts of convective mixing and associated meso-scale dynamics of the local boundary layer and local human activities; all modulated by synoptic meteorology, biomass burning and urban activities in producing the observed spatiality and seasonality 45,48,51,79,85,107,108,[122][123][124][125] .…”
Section: Spatial Synthesis Observations and Modelsmentioning
confidence: 99%