2018
DOI: 10.1134/s1024856018020124
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Siberian Smoke Haze over European Territory of Russia in July 2016: Atmospheric Pollution and Radiative Effects

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Cited by 24 publications
(4 citation statements)
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“…Studying the distribution of the absorbing substance over the size spectrum of atmospheric aerosol is important for the development of correct models for calculating radiation-relevant optical characteristics, primarily the aerosol single scattering albedo in the visible wavelength range. This parameter determines the role of aerosols in the atmosphere as a cooling or warming factor, causing aerosol radiation forcing in the atmosphere and climate change [36][37][38][39][40][41][42]. Information about the equivalent black carbon (EBC) size distribution is also necessary for correct estimates of the mass of absorbing substances falling to the surface at various distances from remote sources of industrial pollution and smoke from wildfires, including in the Arctic region [38,[43][44][45].…”
Section: Analysis Of the Size Distribution Of The Absorbing Substancementioning
confidence: 99%
“…Studying the distribution of the absorbing substance over the size spectrum of atmospheric aerosol is important for the development of correct models for calculating radiation-relevant optical characteristics, primarily the aerosol single scattering albedo in the visible wavelength range. This parameter determines the role of aerosols in the atmosphere as a cooling or warming factor, causing aerosol radiation forcing in the atmosphere and climate change [36][37][38][39][40][41][42]. Information about the equivalent black carbon (EBC) size distribution is also necessary for correct estimates of the mass of absorbing substances falling to the surface at various distances from remote sources of industrial pollution and smoke from wildfires, including in the Arctic region [38,[43][44][45].…”
Section: Analysis Of the Size Distribution Of The Absorbing Substancementioning
confidence: 99%
“…As wildfires in the northern regions increase, the long-range transport of wildfire plumes from central Siberia to Arctic regions can become more common, increasing the impact of carbonaceous aerosols in the Arctic on radiative forcing (Calì Quaglia et al, 2022;Yue et al, 2022). Siberian wildfire plumes may even reach densely populated regions in Europe or East Asia (Ikeda and Tanimoto, 2015;Semoutnikova et al, 2018); this is associated with a significantly increased risk of mortality as well as respiratory and cardiovascular diseases of the exposed population (Chen et al, 2021). Although northern boreal regions like Siberia are predicted to be impacted the most by increasing wildfire intensity, studies investigating organic aerosol emissions, especially from Siberia, are scarce (Flannigan et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…They generally have diameters between 0.001 and 100 µm. Atmospheric aerosols are mainly derived from human activities [5][6][7][8][9] (such as petrochemical fuel use, industrial exhaust emissions) and natural production [7,10]. Aerosols affect atmospheric visibility and human health [11][12][13].…”
Section: Introductionmentioning
confidence: 99%
“…High-intensity human activities also cause the release of a large amount of harmful particulate matter into the atmosphere, seriously affecting air quality and human health. Studying the relationship between AOD and urbanization is of great significance for maintaining and improving the quality of the atmospheric environment [6,[8][9][10]17,[33][34][35][36].…”
Section: Introductionmentioning
confidence: 99%