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AGU: Geophysical Research Letters

 

Keywords

  • aerosol radiative forcing
  • aerosol effects in UV-B

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Pollution: urban and regional
  • Atmospheric Composition and Structure: Radiation: transmission and scattering
  • Atmospheric Composition and Structure: Instruments and techniques

Abstract

Aerosol effects in the UV-B spectral region over Pune, an urban site in India

A. S. Panicker

Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology, Pune, India

G. Pandithurai

Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology, Pune, India

T. Takamura

CEReS, Chiba University, Chiba, Japan

R. T. Pinker

Department of Atmospheric and Ocean Science, University of Maryland, College Park, Maryland, USA

Collocated measurements of UV-B irradiance and aerosol optical characteristics have been carried out over Pune, western India from April 2004 to March 2005 to estimate the role of aerosols in UV-B radiation at the surface. It is found that a unit increases in aerosol optical depth reduces by about 40–56% of the harmful UV-B radiation that reaches the site. Ultraviolet-impact on human health is usually characterized by the UV-index (UV-I), and is estimated with the aid of a radiative transfer model using aerosol and ozone measurements over the site. The index is found to be in the extreme range (10.1 to 13.5) during pre-monsoon, high to extreme (8.5 to 11) during post- monsoon and high (7 to 10) during the winter seasons, vulnerable to sensitive skin. The estimated UV-I values are found to be compared well with SCIAMACHY satellite observed UV-I values with mean ratio of 0.95 ± 0.05.

Received 6 February 2009; accepted 13 April 2009; published 19 May 2009.

Citation: Panicker, A. S., G. Pandithurai, T. Takamura, and R. T. Pinker (2009), Aerosol effects in the UV-B spectral region over Pune, an urban site in India, Geophys. Res. Lett., 36, L10802, doi:10.1029/2009GL037632.

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