Affiliations 

  • 1 DST-Mahamana Centre of Excellence in Climate Change Research, Banaras Hindu University, Varanasi, India. Electronic address: kameshvinjamuri@gmail.com
  • 2 Institute of Environment and Sustainable Development, Banaras Hindu University, Varanasi, India. Electronic address: alaa.mhawish@bhu.ac.in
  • 3 DST-Mahamana Centre of Excellence in Climate Change Research, Banaras Hindu University, Varanasi, India; Institute of Environment and Sustainable Development, Banaras Hindu University, Varanasi, India. Electronic address: tirthankaronline@gmail.com
  • 4 NASA Ames Research Center, Moffett Field, CA, USA. Electronic address: meytar.sorekhamer@nasa.gov
  • 5 Civil and Environmental Engineering, Technion, Hafia, Israel. Electronic address: dbroday@cv.technion.ac.il
  • 6 DST-Mahamana Centre of Excellence in Climate Change Research, Banaras Hindu University, Varanasi, India; Institute of Environment and Sustainable Development, Banaras Hindu University, Varanasi, India. Electronic address: rkmall@bhu.ac.in
  • 7 Center for Earth Sciences and Environment, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, Bangi, Malaysia. Electronic address: talib@ukm.edu.my
Environ Pollut, 2020 Feb;257:113377.
PMID: 31672363 DOI: 10.1016/j.envpol.2019.113377

Abstract

Attenuated backscatter profiles retrieved by the space borne active lidar CALIOP on-board CALIPSO satellite were used to measure the vertical distribution of smoke aerosols and to compare it against the ECMWF planetary boundary layer height (PBLH) over the smoke dominated region of Indo-Gangetic Plain (IGP), South Asia. Initially, the relative abundance of smoke aerosols was investigated considering multiple satellite retrieved aerosol optical properties. Only the upper IGP was selectively considered for CALIPSO retrieval based on prevalence of smoke aerosols. Smoke extinction was found to contribute 2-50% of the total aerosol extinction, with strong seasonal and altitudinal attributes. During winter (DJF), smoke aerosols contribute almost 50% of total aerosol extinction only near to the surface while in post-monsoon (ON) and monsoon (JJAS), relative contribution of smoke aerosols to total extinction was highest at about 8 km height. There was strong diurnal variation in smoke extinction, evident throughout the year, with frequent abundance of smoke particles at lower height (<4 km) during daytime compared to higher height during night (>4 km). Smoke injection height also varied considerably during rice (ON: 0.71 ± 0.65 km) and wheat (AM: 2.34 ± 1.34 km) residue burning period having a significant positive correlation with prevailing PBLH. Partitioning smoke AOD against PBLH into the free troposphere (FT) and boundary layer (BL) yield interesting results. BL contribute 36% (16%) of smoke AOD during daytime (nighttime) and the BL-FT distinction increased particularly at night. There was evidence that despite travelling efficiently to FT, major proportion of smoke AOD (50-80%) continue to remain close to the surface (<3 km) thereby, may have greater implications on regional climate, air quality, smoke transport and AOD-particulate modelling.

* Title and MeSH Headings from MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine.