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Aerosol particle behavior during Dust Storm and Diwali over an urban location in north western India

Author

Listed:
  • Divya Prakash
  • Swagata Payra
  • Sunita Verma
  • Manish Soni

Abstract

In this study, the aerosol behavior during two contradictory events, i.e., dust storm (DS) and Diwali (DW) has been studied over Jaipur. The aerosol particle number concentration shows distinct features between DS and DW events. The total ANC was found minimum during DS while maximum during DW. The 24 h mean of total ANC was 9.15 × 10 4 (±7.71 × 10 4 ) and 5.38 × 10 5 (±3.73 × 10 5 particles/l) during DS and DW, respectively. The total ANC increases from 7.78 × 10 4 to 5.32 × 10 5 and 3.52 × 10 5 to 1.70 × 10 6 particles/l in 24 h during DS and DW, respectively. In DS, the ANC in coarse mode (2 > particle diameter > 20 μm) is significantly high while in DW, the ANC in fine mode (0.3 > particle diameter > 2 μm) exhibits higher concentration. During dust episode, a significant change in ANC (3.0 × 10 3 to 1.12 × 10 5 particles/l) was observed for the particle of size range in 2.0–20 μm with a slight increase in particles number concentration (7.48 × 10 4 to 4.20 × 10 5 particles/l) in 0.3–2.0 μm range is also observed. During DS, the fine and coarse mode particles increased 4.61 and 36.44 times while during DW, it increased 3.83 and 0.95 times, respectively. The relatively high particle levels during DW are attributed for two reasons: local emissions due to burning of fire crackers and meteorological conditions, i.e., low wind speeds and low mixing-layer heights lead to relatively high particle concentrations. Copyright Springer Science+Business Media Dordrecht 2013

Suggested Citation

  • Divya Prakash & Swagata Payra & Sunita Verma & Manish Soni, 2013. "Aerosol particle behavior during Dust Storm and Diwali over an urban location in north western India," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 69(3), pages 1767-1779, December.
  • Handle: RePEc:spr:nathaz:v:69:y:2013:i:3:p:1767-1779
    DOI: 10.1007/s11069-013-0780-1
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