Abstract

The tropospheric NO2 concentration from OMI AURA always shows high concentrations of NO2 at a few locations in India, one of the high concentrations of NO2 hotspots is associated with the locations of seven coal-fired Thermal Power plants (TPPs) in Singrauli. Emissions from TPPs are among the major sources of black carbon (BC) soot in the atmosphere. Knowledge of BC emissions from TPPs is important in characterizing regional carbonaceous particulate emissions, understanding the fog/haze/smog formation, evaluating regional climate forcing, modeling aerosol optical parameters and concentrations of black carbon, and evaluating human health. Furthermore, elevated BC concentrations, over the Indo-Gangetic Plain (IGP) and the Himalayan foothills, have emerged as an important subject to estimate the effects of deposition and atmospheric warming of BC on the accelerated melting of snow and glaciers in the Himalaya. For the first time, this study reports BC concentrations and aerosol optical parameters near dense coal-fired power plants and open cast coal mining adjacent to the east IGP. In-situ measurements were carried out in Singrauli (located in south-east IGP) at a fixed site about 10 km from power plants and in transit measurements in close proximity to the plants, for few days in the month of January and March 2013. At the fixed site, BC concentration up to the 95 μgm−3 is observed with strong diurnal variations. BC concentration shows two maxima peaks during early morning and evening hours. High BC concentrations are observed in close proximity to the coal-fired TPPs (>200 μgm−3), compared to the outside domain of our study region. Co-located ground-based sunphotometer measurements of aerosol optical depth (AOD) show strong spatial variability at the fixed site, with AOD in the range 0.38–0.58, and the highest AOD in the range 0.7–0.95 near the TPPs in transit measurements (similar to the peak of BC concentrations). Additionally, the Angstrom exponent was found to be in the range 0.4–1.0 (maximum in the morning time) and highest in the proximity of TPPs (~1.0), suggesting abundance of fine particulates, whereas there was low Angstrom exponent over the surrounding coal mining areas. Low Angstrom exponent is characterized by dust from the unpaved roads and nearby coal mining areas. MODIS derived daily AOD shows a good match with the MICROTOPS AOD. The CALIPSO derived subtypes of the aerosol plot shows that the aerosols over Singrauli region are mainly dust, polluted dust, and elevated smoke. The preliminary study for few days provides information about the BC concentrations and aerosol optical properties from Singrauli (one of the NO2 hotspot locations in India). This preliminary study suggests that long-term continuous monitoring of BC is needed to understand the BC concentrations and aerosol optical properties for better quantification and the estimation of the emission to evaluate radiative forcing in the region.

Highlights

  • Incomplete combustion of fossil fuels, various types of biomass/biofuels in small-scale residential cooking and heating activities, and large forest fires/crops residue burning release huge amounts of black carbon (BC) aerosols [1,2,3,4]

  • The 24-h continuous measurement of BC concentration at the fixed site is shown in Figure 4 for the two different campaigns during winter (13 January) and pre-monsoon season (27 March)

  • Similar variation was recorded for the March but the morning and evening peak was less prominent, due to the change in boundary layer height and less calm environment, which allows for diffusing the pollutants for long distances and heights

Read more

Summary

Introduction

Incomplete combustion of fossil fuels, (e.g., diesel and coal), various types of biomass/biofuels in small-scale residential cooking and heating activities, and large forest fires/crops residue burning release huge amounts of black carbon (BC) aerosols [1,2,3,4]. Black carbon emissions are considered as particles, not a greenhouse gas, and they are the second or third largest climate warmer after carbon dioxide [5,6]. The BC emission has attracted the interests of scientists due to its different anthropogenic sources and adverse effect on climate and environment [7]. The uncertainties in the climate forcing from black carbon aerosol are largely due to inadequate study and measurements of cloud interaction with the co-emitted organic carbon [6]. The main removal mechanism of BC from the atmosphere is the wet deposition [10]

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call