Exercise has been proved to promote the number and activity of circulating endothelial progenitor cells (EPCs) in humans, which contributes to improvement in endothelial function and maintenance of cardiovascular homoeostasis. However, the mechanism underlying the effect of exercise on circulating EPCs in healthy subjects is not completely understood. Here, we investigated whether the regulation of acute exercise on circulating EPCs is associated with nitric oxide (NO), vascular endothelial growth factors (VEGF) and granulocyte macrophage colony stimulating factor (GM-CSF) known to modulate circulating EPCs in healthy subjects. A total of 16 healthy male volunteers underwent a modified Bruce treadmill acute exercise protocol. The number and activity of circulating EPCs, as well as the levels of NO-VEGF and GM-CSF in plasma and culture medium before and after exercise in healthy subjects were measured. The number and activity of circulating EPCs after acute exercise were significantly higher than those before exercise in healthy subjects. In parallel, acute exercise significantly enhanced plasma NO level in healthy subjects. There is a significant linear regression relationship between the enhanced plasma NO level and increased number or activity of circulating EPCs. However, no change of plasma VEGF and GM-CSF level was observed after acute exercise. The secretion of NO-VEGF and GM-CSF by cultured EPCs remained unchanged in response to acute exercise. The present study demonstrates for the first time that acute exercise-induced NO production contributes to upregulation of circulating EPCs in healthy subjects, which suggests that NO plays an important role in the regulation of exercise on circulating EPCs.

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Secondary organic aerosol (SOA) constitutes a large fraction of organic aerosol worldwide, however, the formation mechanisms in polluted environments remain poorly understood. Here we observed fast daytime growth of oxygenated organic aerosol (OOA) (with formation rates up to 10 μg m −3 h −1 ) during low relative humidity (RH, daytime average 38 ± 19%), high RH (53 ± 19%), and fog periods (77 ± 13%, fog occurring during nighttime with RH reaching 100%). Evidence showed that photochemical aqueous-phase SOA (aqSOA) formation dominantly contributed to daytime OOA formation during the periods with nighttime fog, while both photochemical aqSOA and gas-phase SOA (gasSOA) formation were important during other periods with the former contributing more under high RH and the latter under low RH conditions, respectively. Compared to daytime photochemical aqSOA production, dark aqSOA formation was only observed during the fog period and contributed negligibly to the increase in OOA concentrations due to fog scavenging processes. The rapid daytime aging, as indicated by the rapid decrease in m,p-xylene/ethylbenzene ratios, promoted the daytime formation of precursors for aqSOA formation, e.g., carbonyls such as methylglyoxal. Photooxidants related to aqSOA formation such as OH radical and H 2 O 2 also bear fast daytime growth features even under low solar radiative conditions. The simultaneous increases in ultraviolet radiation, photooxidant, and aqSOA precursor levels worked together to promote the daytime photochemical aqSOA formation. We also found that biomass burning emissions can promote photochemical aqSOA formation by adding to the levels of aqueous-phase photooxidants and aqSOA precursors. Therefore, future mitigation of air pollution in a polluted environment would benefit from stricter control on biomass burning especially under high RH conditions.

Abstract. Aerosol hygroscopicity is crucial for understanding roles of aerosol particles in atmospheric chemistry and aerosol climate effects. Light-scattering enhancement factor f (RH, λ) is one of the parameters describing aerosol hygroscopicity, which is defined as f (RH, λ) = σ sp (RH, λ)/σ sp (dry, λ), where σ sp (RH, λ) or σ sp (dry, λ) represents σ sp at wavelength λ under certain relative humidity (RH) or dry conditions. Traditionally, an overall hygroscopicity parameter κ can be retrieved from measured f (RH, λ), hereinafter referred to as κ f (RH) , by combining concurrently measured particle number size distribution (PNSD) and mass concentration of black carbon. In this paper, a new method is proposed to directly derive κ f (RH) based only on measurements from a three-wavelength humidified nephelometer system. The advantage of this newly proposed approach is that κ f (RH) can be estimated without any additional information about PNSD and black carbon. This method is verified with measurements from two different field campaigns. Values of κ f (RH) estimated from this new method agree very well with those retrieved by using the traditional method: all points lie near the 1 : 1 line and the square of correlation coefficient between them is 0.99. The verification results demonstrate that this newly proposed method of deriving κ f (RH) is applicable at different sites and in seasons of the North China Plain and might also be applicable in other regions around the world.

Abstract. The aim of this investigation was to obtain a better understanding of the variability of the cloud condensation nuclei (CCN) activity during new particle formation (NPF) events in an anthropogenically polluted atmosphere of the North China Plain (NCP). We investigated the size-resolved activation ratio as well as particle number size distribution, hygroscopicity, and volatility during a 4-week intensive field experiment in summertime at a regional atmospheric observatory in Xianghe. Interestingly, based on a case study, two types of NPF events were found, in which the newly formed particles exhibited either a higher or a lower hygroscopicity. Therefore, the CCN activity of newly formed particles in different NPF events was largely different, indicating that a simple parameterization of particle CCN activity during NPF events over the NCP might lead to poor estimates of CCN number concentration (NCCN). For a more accurate estimation of the potential NCCN during NPF events, the variation of CCN activity has to be taken into account. Considering that a fixed activation ratio curve or critical diameter are usually used to calculate NCCN, the influence of the variation of particle CCN activity on the calculation of NCCN during NPF events was evaluated based on the two parameterizations. It was found that NCCN might be underestimated by up to 30 % if a single activation ratio curve (representative of the region and season) were to be used in the calculation; and might be underestimated by up to 50 % if a fixed critical diameter (representative of the region and season) were used. Therefore, we suggest not using a fixed critical diameter in the prediction of NCCN in NPF. If real-time CCN activity data are not available, using a proper fixed activation ratio curve can be an alternative but compromised choice.