Seasonal variation of near surface black carbon and satellite derived vertical distribution of aerosols over a semi-arid station in India

Kalluri, Raja Obul Reddy ; Gugamsetty, Balakrishnaiah ; Kotalo, Rama Gopal ; Nagireddy, Siva Kumar Reddy ; Tandule, Chakradhar Rao ; Thotli, Lokeswara Reddy ; Shaik, Nazeer Hussain ; Maraka, Vasudeva Reddy ; Rajuru, Ramakrishna Reddy ; Surendran Nair, Suresh Babu (2017) Seasonal variation of near surface black carbon and satellite derived vertical distribution of aerosols over a semi-arid station in India Atmospheric Research, 184 . pp. 77-87. ISSN 0169-8095

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Official URL: http://doi.org/10.1016/j.atmosres.2016.09.003

Related URL: http://dx.doi.org/10.1016/j.atmosres.2016.09.003

Abstract

Extensive measurements of aerosol black carbon mass concentration (BC) and vertical profiles of atmospheric aerosols have been carried out using Aethalometer and CALIPSO level – 2 satellite data from December 2012 to November 2014 over a semi-arid station, Anantapur. We found a bimodal distribution in the mass concentrations of BC aerosols on a diurnal scale. A sharp peak was observed during morning rush hours (7:00 to 8:00 LT) almost an hour after the local sunrise. After which, a broad nocturnal peak was found during ~ 21:00 to 22:00 LT. The seasonal mean BC concentrations (Mixed layer height (ML)) were found to be 3.45 ± 1.44 μg/m3 (676 ± 117 m), 2.55 ± 0.85 μg/m3 (1215 ± 190 m), 1.22 ± 0.31 μg/m3 (1134 ± 194 m) and 1.75 ± 0.70 μg/m3 (612 ± 135 m), during the winter, summer, monsoon and post-monsoon respectively. The vertical profiles of aerosol extinction coefficient and back scattering ratio profiles were derived from Cloud Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) showed a strong seasonal variation with aerosols mostly confined below 2 km during the post-monsoon and winter seasons whereas in the other two seasons, the aerosol layer expands beyond 6 km. Depolarization ratios (> 0.2) are higher during summer and monsoon at higher altitude regions demonstrate the presence of dust particles, which contribute to the large aerosol extinction at higher levels. These results are further supported by the backward trajectory cluster analysis.

Item Type:Article
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