B. Suresh Kumar Reddy
Sri Krishnadevaraya University
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Science of The Total Environment | 2009
K. Raghavendra Kumar; K. Narasimhulu; G. Balakrishnaiah; B. Suresh Kumar Reddy; K. Rama Gopal; R.R. Reddy; K. Krishna Moorthy; S. Suresh Babu
Regular measurements of size segregated as well as total mass concentration and size distribution of near surface composite aerosols, made using a ten-channel Quartz Crystal Microbalance (QCM) cascade impactor during the period of September 2007-May 2008 are used to study the aerosol characteristics in association with the synoptic meteorology. The total mass concentration varied from 59.70+/-1.48 to 41.40+/-1.72 microg m(-3), out of which accumulation mode dominated by approximately 50%. On a synoptic scale, aerosol mass concentration in the accumulation (submicron) mode gradually increased from an average low value of approximately 26.92+/-1.53 microg m(-3) during the post monsoon season (September-November) to approximately 34.95+/-1.32 microg m(-3) during winter (December-February) and reaching a peak value of approximately 43.56+/-1.42 microg m(-3) during the summer season (March-May). On the contrary, mass concentration of aerosols in the coarse (supermicron) mode increased from approximately 9.23+/-1.25 microg m(-3)during post monsoon season to reach a comparatively high value of approximately 25.89+/-1.95 microg m(-3) during dry winter months and a low value of approximately 8.07+/-0.76 microg m(-3) during the summer season. Effective radius, a parameter important in determining optical (scattering) properties of aerosol size distribution, varied between 0.104+/-0.08 microm and 0.167+/-0.06 microm with a mean value of 0.143+/-0.01 microm. The fine mode is highly reduced during the post monsoon period and the large and coarse modes continue to remain high (replenished) so that their relative dominance increases. It can be seen that among the two parameters measured, correlation of total mass concentration with air temperature is positive (R(2)=0.82) compared with relative humidity (RH) (R(2)=0.75).
Atmospheric Research | 2011
K. Raghavendra Kumar; K. Narasimhulu; G. Balakrishnaiah; B. Suresh Kumar Reddy; K. Rama Gopal; R.R. Reddy; S. K. Satheesh; K. Krishna Moorthy; S. Suresh Babu
Atmospheric Research | 2010
B. Suresh Kumar Reddy; K. Raghavendra Kumar; G. Balakrishnaiah; K. Rama Gopal; R.R. Reddy; Y. Nazeer Ahammed; K. Narasimhulu; L. Siva Sankara Reddy; S. Lal
Aerosol and Air Quality Research | 2012
B. Suresh Kumar Reddy; K. Raghavendra Kumar; G. Balakrishnaiah; K. Rama Gopal; R.R. Reddy; Venkataraman Sivakumar; A.P. Lingaswamy; S.Md. Arafath; K. Umadevi; S. Pavan Kumari; Y. Nazeer Ahammed; S. Lal
Aerosol and Air Quality Research | 2012
B. Suresh Kumar Reddy; K. Raghavendra Kumar; G. Balakrishnaiah; K. Rama Gopal; R.R. Reddy; L.S.S. Reddy; Y. Nazeer Ahammed; K. Narasimhulu; K. Krishna Moorthy; S. Suresh Babu
Atmospheric Environment | 2012
G. Balakrishnaiah; K. Raghavendra Kumar; B. Suresh Kumar Reddy; K. Rama Gopal; R.R. Reddy; L.S.S. Reddy; C. Swamulu; Y. Nazeer Ahammed; K. Narasimhulu; K. Krishnamoorthy; S. Suresh Babu
Atmospheric Environment | 2011
G. Balakrishnaiah; K. Raghavendra Kumar; B. Suresh Kumar Reddy; K. Rama Gopal; R.R. Reddy; L.S.S. Reddy; Y. Nazeer Ahammed; K. Narasimhulu; K. Krishna Moorthy; S. Suresh Babu
Journal of Asian Earth Sciences | 2011
G. Balakrishnaiah; K. Raghavendra Kumar; B. Suresh Kumar Reddy; C. Swamulu; K. Rama Gopal; R.R. Reddy; L.S.S. Reddy; Y. Nazeer Ahammed; K. Narasimhulu; K. Krishnamoorthy; S. Suresh Babu
Journal of Atmospheric and Solar-Terrestrial Physics | 2011
B. Suresh Kumar Reddy; K. Raghavendra Kumar; G. Balakrishnaiah; K. Rama Gopal; R.R. Reddy; L.S.S. Reddy; K. Narasimhulu; S. Vijaya Bhaskara Rao; T. Kiran Kumar; C. Balanarayana; K. Krishna Moorthy; S. Suresh Babu
Atmospheric Research | 2010
K. Raghavendra Kumar; K. Narasimhulu; G. Balakrishnaiah; B. Suresh Kumar Reddy; K. Rama Gopal; R.R. Reddy; S. K. Satheesh; K. Krishna Moorthy; S. Suresh Babu