2016
DOI: 10.1016/j.atmosenv.2015.11.023
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Dry deposition of particulate matter at an urban forest, wetland and lake surface in Beijing

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Cited by 79 publications
(51 citation statements)
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“…Although the anthropogenic emissions may be significantly reduced during nighttime, the boundary layer height at night is typically low and the wind speed is low (Table 2), which limits the diffusion of air pollutants and leads to a rise in the concentrations. Moreover, the stagnant meteorological conditions during nighttime are unfavorable to the dry deposition of fine particles, especially those in accumulation mode [47]. As a result, the concentration of primary EC during nighttime was 1.5 times what it was during daytime.…”
Section: Day-night Differencesmentioning
confidence: 82%
“…Although the anthropogenic emissions may be significantly reduced during nighttime, the boundary layer height at night is typically low and the wind speed is low (Table 2), which limits the diffusion of air pollutants and leads to a rise in the concentrations. Moreover, the stagnant meteorological conditions during nighttime are unfavorable to the dry deposition of fine particles, especially those in accumulation mode [47]. As a result, the concentration of primary EC during nighttime was 1.5 times what it was during daytime.…”
Section: Day-night Differencesmentioning
confidence: 82%
“…On the one hand, PM 2.5 was significantly affected by natural factors such as climate, topography, and surface vegetation [42,43,44] besides socio-economic drivers. C year is a combined effect of these factors.…”
Section: Discussionmentioning
confidence: 99%
“…in which U(z) (m·s −1 ) is the average wind velocity; u* (m·s −1 ) is friction velocity which can be directly measured; k is the von Karman constant (0.41); d (m) is displacement height; Z 0 is roughness length, which is used to model the horizontal mean wind speed near the ground and is equivalent to the height at which the wind speed theoretically becomes zero [19], according to Zhang et al (2001) [20], Z 0 was determined by considering different seasons and land use categories-in our study, Z 0 was 0.75 at Olympic Forest Park and 0.8 at Jiufeng National Forest Park. The value of d can be calculated by iterative method [18] as:…”
Section: Calculation Of Deposition Velocitymentioning
confidence: 99%