Vertical profiles of black carbon aerosols over the urban locations in South India

Vertical profiles of black carbon (BC) aerosol were determined from aircraft measurements under the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX) program conducted by the Indian Institute of Tropical Meteorology, India during 2009 over Bangalore and Hyderabad in south...

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Published inThe Science of the total environment Vol. 431; pp. 323 - 331
Main Authors Safai, P.D., Raju, M.P., Maheshkumar, R.S., Kulkarni, J.R., Rao, P.S.P., Devara, P.C.S.
Format Journal Article
LanguageEnglish
Published Kidlington Elsevier B.V 01.08.2012
Elsevier
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Summary:Vertical profiles of black carbon (BC) aerosol were determined from aircraft measurements under the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX) program conducted by the Indian Institute of Tropical Meteorology, India during 2009 over Bangalore and Hyderabad in south India. BC mass loadings decreased approximately monotonically from 103 to 104ng/m3 at the surface to ~102ng/m3 at an altitude of about 7km; although layers at intermediate levels containing anomalously high BC loadings were frequently encountered that were attributed mainly to the convective transport from surface sources accompanied by changes in the local boundary layer and atmospheric stability. In addition, as evidenced from air mass back trajectories; long range transport from distant sources contributed to some anomalous spikes in BC concentration. The presence of BC in cloud forming regions of the free troposphere could have important implications for cloud microphysics and subsequent rainfall mechanism over this region. Apart from this, the effects on human health are equally important. ► Vertical profiles of black carbon (BC) aerosols were obtained for the first time up to 7km over India. ► BC concentration decreased with increasing height though layers of elevated concentration observed at different altitudes. ► Local surface sources and remote sources contribute to the observed BC concentrations.
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ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2012.05.058