2016
DOI: 10.1016/j.atmosenv.2015.07.031
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Aerosol chemical characterization and role of carbonaceous aerosol on radiative effect over Varanasi in central Indo-Gangetic Plain

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Cited by 63 publications
(25 citation statements)
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References 105 publications
(171 reference statements)
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“…The coarse-mode (PM 10-2.5 ) fraction was ∼ 60 % of the PM 10 . The share of coarse-mode aerosol to PM 10 in Lumbini was higher than that observed in other sites in the IGP, such as Guwahiti, India (42 %) (Tiwari et al, 2017), and Dibrugarh, India (9-16 %) (Pathak et al, 2013), both in eastern IGP and Delhi (38 %) in western IGP, indicating the higher contribution of coarse aerosols in Lumbini, likely lifted from soils from nearby agricultural fields and construction materials by stronger winds during pre-monsoon season.…”
Section: Meteorologycontrasting
confidence: 61%
See 1 more Smart Citation
“…The coarse-mode (PM 10-2.5 ) fraction was ∼ 60 % of the PM 10 . The share of coarse-mode aerosol to PM 10 in Lumbini was higher than that observed in other sites in the IGP, such as Guwahiti, India (42 %) (Tiwari et al, 2017), and Dibrugarh, India (9-16 %) (Pathak et al, 2013), both in eastern IGP and Delhi (38 %) in western IGP, indicating the higher contribution of coarse aerosols in Lumbini, likely lifted from soils from nearby agricultural fields and construction materials by stronger winds during pre-monsoon season.…”
Section: Meteorologycontrasting
confidence: 61%
“…In Lumbini, the average (hourly) share of PM 1 in PM 2.5 , PM 1 in PM 10 and PM 2.5 in PM 10 was found to be ∼ 70, 34 and 47 %, respectively. Regarding other sites in IGP region, PM 2.5 / PM 10 ratios were reported to be 56 % in Kanpur (Snider et al, 2016), 60 % in Varanasi (Kumar et al, 2015), 57 % in Guwahiti (Tiwari et al, 2017), 90 % in Dribugarh (Pathak et al, 2013) and 62 % in Delhi , indicating local differences within IGP as well as suggesting that the influence of combustion sources at Lumbini is still lower compared to other locations in the Indian section of the IGP. A recent study (Putero et al, 2015) reported that the PM 1 / PM 10 during pre-monsoon of 2013 was found to be 0.39 in the Kathmandu Valley of Nepal.…”
Section: Meteorologymentioning
confidence: 97%
“…The contribution of BC in PM 1 was found to be ∼ 12 % in Kanpur during February-March (Kumar et al, 2016a), similar to Lumbini. Regarding the share of BC in PM 10 , the share observed in Lumbini (∼ 4 %) was similar to that observed over Varanasi (∼ 340 km south of our site) in central IGP (5 %) (Tiwari et al, 2016) and Dibrugarh in eastern IGP (∼ 5 %) (Pathak et al, 2013). Thus our results indicate that despite our station being located at the northern edge of the IGP along the foothills of the Himalayan range, the share of BC in PM is similar to that found in heavily polluted sites in the central and eastern IGP.…”
Section: Meteorologymentioning
confidence: 52%
“…The higher concentrations found in the intensive campaigns have already been attributed to biomass burning in previous studies (Pereira et al, 2017;Vasconcellos et al, 2011a). However, potassium ions can also come from soil resuspension (Ram et al, 2010;Tiwari et al, 2016), which becomes important in PM 2.5−10 . Higher concentrations of chloride in fine particles (964 and 330 ng m −3 for Int 2.5 and Ext 2.5 , respectively) were observed in the Int 2.5 campaign (although the value of p was slightly above 0.05), probably due to a higher influence of biomass burning .…”
Section: Wsi and Trace Elementsmentioning
confidence: 87%