4.7 Article

What caused severe air pollution episode of November 2016 in New Delhi?

Journal

ATMOSPHERIC ENVIRONMENT
Volume 222, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2019.117125

Keywords

Biomass burning; Severe air pollution episode; Particulate matter; Indo-Gangetic plain

Funding

  1. University Grants Commission, Government of India [F.4-5(230-FRP/2015/BSR)]
  2. DST-SERB [ECR/2016/001333]
  3. DST SERB [ECR/2015/000490]

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In recent years, South Asia is experiencing severely degraded air quality, with particulate matter less than 2.5 mu m (PM2.5) reaching unprecedented high levels. Here, we investigate a severe air pollution episode (SAPE) witnessed in New Delhi during 1-7 November 2016. This was a very unusual air pollution episode wherein air quality index exceeded >500 and was persistent for about a week encapsulating the entire Indo-Gangetic Plain (IGP). We demonstrate that a stagnant weather condition was the dominant cause of the SAPE. Mean concentration of PM2.5 in New Delhi before, during, and after the SAFE were 142 mu g/m(3), 563 mu g/m(3), and 240 mu g/m(3), respectively. Satellite-based aerosol optical depth (AOD), ultraviolet-aerosol index (UV-AI) and surface carbon monoxide (CO) concentrations also showed significant enhancements over large locale spatially by about 50-70% during the SAPE. A large and simultaneous increase in UV-AI and CO downwind of a large number of fire hotspots (Punjab and Haryana) is a clear indication of biomass burning aerosols. Analysis of absorption Angstrom exponent further substantiates this finding, showing a large fraction of light absorbing carbonaceous-type aerosols. Radiosonde observations clearly showed that stagnant atmospheric conditions led to SAPE in New Delhi by allowing pollution to accumulate and persist in the near-surface environment. As a result new particle formation was suppressed due to very high pre-existing aerosol concentrations during the SAPE. The heating rate induced by light absorbing aerosols into an atmospheric layer during SAPE was also very high (3.1 +/- 0.7 K/day). These findings will help in understanding air quality and climate effects, as well as in formulating policies to mitigate these complex pollution episodes in an anthropogenic future.

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