2018
DOI: 10.1016/j.atmosres.2018.05.005
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Characterizing the level, photochemical reactivity, emission, and source contribution of the volatile organic compounds based on PTR-TOF-MS during winter haze period in Beijing, China

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Cited by 79 publications
(61 citation statements)
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“…where PA and VMR are the primary anthropogenic component and the total volume mixing ratio of a given VOC (Brito et al, 2015;Sheng et al, 2018). As discussed above, the ERs derived from nighttime data are still applicable during the whole day.…”
Section: Anthropogenic and Biogenic/secondary Contribution To Ovocsmentioning
confidence: 99%
“…where PA and VMR are the primary anthropogenic component and the total volume mixing ratio of a given VOC (Brito et al, 2015;Sheng et al, 2018). As discussed above, the ERs derived from nighttime data are still applicable during the whole day.…”
Section: Anthropogenic and Biogenic/secondary Contribution To Ovocsmentioning
confidence: 99%
“…The wind direction also seemed to be cyclical on each day in response to local mountain valley circulation around Beijing (Hu et al, 2005). According to other studies, stronger northerly winds occurring in the winter are the main mechanism through which pollution is removed, leading to good air quality (Sheng et al, 2018).…”
Section: Surface Observations Of Haze and Meteorological Conditionsmentioning
confidence: 89%
“…The potential temperature (θ ) determined by radiosonde technology is calculated from the following formula: (Stull, 1988); T is the measured temperature. As noted in many previous stud-ies, the most widely used approach for the determination of the ABL height and structure for the daytime and nighttime involves identifying local maxima in potential temperature vertical gradient profiles as measured by radiosonde devices (Seibert et al, 2000;Summa et al, 2013;Sorbjan, 1989), but this method is only appropriate to apply to the convective ABL (Hennemuth and Lammert, 2006). Since the pollution period we examine involves stagnant winter weather conditions and as our radiosonde data only apply to dawn and dusk periods (08:00 and 20:00 LT), a stable boundary layer often appears (see Fig.…”
Section: Boundary Layer Structure Observed By Radiosonde Technologiesmentioning
confidence: 99%
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“…The most predominant atmospheric carbonyl compounds besides formaldehyde are acetaldehyde and acetone. They have been reported to vary from a few hundred ppt in remote areas (Warneke and de Gouw, 2001; Lewis et al, 2005;White et al, 2008;Colomb et al, 2009;Read et al, 2012;Sjostedt et al, 2012;Tanimoto et al, 2014;Hornbrook et al, 2016) to several ppb in urban and polluted areas (Dolgorouky et al, 2012;Guo et al, 2013;Stoeckenius and McNally, 2014;Sahu et al, 2017;Sheng et al, 2018). Generally, secondary photochemical formation from various precursors is the main source in those regions.…”
Section: Introductionmentioning
confidence: 99%