Variation between near-surface and columnar aerosol characteristics during the winter and summer at Delhi in the Indo-Gangetic Basin
Variation between near-surface and columnar aerosol characteristics during the winter and summer at Delhi in the Indo-Gangetic Basin
| dc.contributor.author | Srivastava, A. K. | |
| dc.contributor.author | Singh, Sachchidanand | |
| dc.contributor.author | Tiwari, S. | |
| dc.contributor.author | Kanawade, V. P. | |
| dc.contributor.author | Bisht, D. S. | |
| dc.date.accessioned | 2022-03-26T23:50:44Z | |
| dc.date.available | 2022-03-26T23:50:44Z | |
| dc.date.issued | 2012-03-01 | |
| dc.description.abstract | Aerosol characteristics were studied over Delhi, a typical urban station in the Ganga basin in Northern India, during two contrasting weather conditions: winter and summer, to explain the changes in columnar and surface aerosol characteristics with the help of ground based measurements and CALIPSO satellite data. The near-surface mean aerosol mass concentrations of PM 10 and PM 2.5 (±standard deviation) were observed to be ~200 (±24) and 118 (±33)μgm -3, respectively, during the winter and ~168 (±31) and 55 (±12)μgm -3, respectively, during the summer. PM 2.5 was found to be about two times higher than the PM 10 concentration during the winter period. Aerosol mass size distribution showed bi-modal nature during both the periods, with relative dominance of fine-particle mass concentrations during the winter, having low R eff value (0.63±0.05μm) and coarse-particle mass concentrations during the summer, having large R eff value (1.52±0.60μm). The concurrent measurement of columnar aerosol optical depth (AOD) showed high values (>0.60 at 500nm) during both the periods. The Ångström exponent (α) over the station, however, also suggests relatively large contribution of fine-mode particles during the winter (α~1.02) and coarse-mode dust particles during the summer (α~0.51). The observed features in the surface and columnar measured aerosol characteristics during two different seasons are explained using the vertical winds coupled with the vertical profile of aerosols. © 2011 Elsevier Ltd. | |
| dc.identifier.citation | Journal of Atmospheric and Solar-Terrestrial Physics. v.77 | |
| dc.identifier.issn | 13646826 | |
| dc.identifier.uri | 10.1016/j.jastp.2011.11.009 | |
| dc.identifier.uri | https://www.sciencedirect.com/science/article/abs/pii/S1364682611003129 | |
| dc.identifier.uri | https://dspace.uohyd.ac.in/handle/1/2749 | |
| dc.subject | Aerosol backscatter | |
| dc.subject | Aerosol optical depth | |
| dc.subject | PM 10 | |
| dc.subject | PM 2.5 | |
| dc.subject | Vertical winds (omega) | |
| dc.title | Variation between near-surface and columnar aerosol characteristics during the winter and summer at Delhi in the Indo-Gangetic Basin | |
| dc.type | Journal. Article | |
| dspace.entity.type |
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