Effects of agriculture crop residue burning on aerosol properties and long-range transport over northern India: A study using satellite data and model simulations

Agriculture crop residue burning in the tropics is a major source of the global atmospheric aerosols and monitoring their long-range transport is an important element in climate change studies. In this paper, we study the effects of agriculture crop residue burning on aerosol properties and long-ran...

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Veröffentlicht in:Atmospheric research 2016-09, Vol.178-179, p.155-163
Hauptverfasser: Vijayakumar, K., Safai, P.D., Devara, P.C.S., Rao, S. Vijaya Bhaskara, Jayasankar, C.K.
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Sprache:eng
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Zusammenfassung:Agriculture crop residue burning in the tropics is a major source of the global atmospheric aerosols and monitoring their long-range transport is an important element in climate change studies. In this paper, we study the effects of agriculture crop residue burning on aerosol properties and long-range transport over northern India during a smoke event that occurred between 09 and 17 November 2013, with the help of satellite measurements and model simulation data. Satellite data observations on aerosol properties suggested transport of particles from agriculture crop residue burning in Indo-Gangetic Plains (IGP) over large regions. Additionally, ECMWF winds at 850hPa have been used to trace the source, path and spatial extent of smoke events. Most of the smoke aerosols, during the study period, travel from a west-to-east pathway from the source-to-sink region. Furthermore, aerosol vertical profiles from CALIPSO show a layer of thick smoke extending from surface to an altitude of about 3km. Smoke aerosols emitted from biomass burning activity from Punjab have been found to be a major contributor to the deterioration of local air quality over the NE Indian region due to their long range transport. •Agricultural crop residue burning enhanced aerosol levels in the IGP.•Satellite and model analysis used to detect smoke aerosols.•Maximum ratios of AI and AOD to columnar NO2 detected during smoke event.•Smoke and dust aerosol layer formed up to 3km in the atmosphere.
ISSN:0169-8095
1873-2895
DOI:10.1016/j.atmosres.2016.04.003