Volume 16, No. 6, June 2016, Pages 1427-1440 PDF(1.51 MB)
Characterisation of Absorbing Aerosols Using Ground and Satellite Data at an Urban Location, Hyderabad
Subin Jose1, Kaundala Niranjan2, Biswadip Gharai1, Pamaraju Venkata Narasimha Rao1, Vijayakumar S. Nair3
1 Atmospheric & Climate Sciences Group, ECSA, NRSC, Balanagar, Hyderabad, India
2 Department of Physics, Andhra University, Andhra Pradesh, India
3 Space Physics Laboratory (SPL), Vikram Sarabhai Space Centre, Trivandrum, India
- Predominant aerosol types are from fossils fuel, anthropogenic emissions.
- BC showed a significant diurnal variation.
- Biomass/dust aerosols in its pure form are not found.
- Aerosols are confined within 2 km from the surface during winter.
In the present study we have attempted to characterize aerosols using their optical properties over a tropical urban location of Hyderabad, India. We have analyzed three years of in-situ data on aerosol absorption from Aethalometer and scattering from Nephelometer measurements. Satellite based absorption measurements from ozone monitoring instrument, absorbing aerosol index are also analyzed to investigate the role of long range transport of dust. Further, the Cloud–Aerosol Lidar Pathfinder Satellite Observations (CALIPSO) data is used to study the vertical extent of aerosol particles as well as their sphericity using its particulate depolarization ratio. The study revealed that irrespective of seasonal variation, local anthropogenic fossil fuel aerosols form the predominant aerosol type over this site. Biomass/dust aerosols in their pure form are not present during the study period; however the spread of frequency distribution of scattering Angstrom exponent and absorption Angstrom exponent suggested their possible existence in mixed condition with local anthropogenic aerosols. The analysis of columnar aerosol absorption data during pre-monsoon period showed the dominance of UV absorbing dust aerosols in the study region. CALIPSO data analysis over study area showed that majority aerosols are confined within 2 km from the surface during winter while in pre-monsoon particles are distributed throughout the profile (~6 km) with extinction coefficient varying between 0.1–0.2 km–1. As the season shift from winter to pre-monsoon a change in sphericity of particle is observed. Cluster mean trajectory analysis revealed that during pre-monsoon majority of air mass movements (~68%) are from western side passing through dust source region like Persian Gulf and Thar Desert before entering into Indian region. During post-monsoon (~70%) and winter (~65%), majority of the air masses are coming from north-west and north-east side of the study area where biomass burning is quite frequent during this period
Absorption coefficient; Angstrom exponent; Black carbon; Aerosol index and particulate depolarization ratio.