Enhancement of nanoparticle formation and growth during the COVID-19 lockdown period in urban Beijing

. Inﬂuenced by the spread of the global 2019 novel coronavirus (COVID-19) pandemic, primary emissions of particles and precursors associated with anthropogenic activities decreased signiﬁcantly in China during the Chinese New Year of 2020 and the lockdown period (24 January–16 February 2020). The 2-month measurements of the number size distribution of neutral particles and charged ions showed that during the lockdown (LCD) period, the number concentration of particles smaller than 100 nm decreased by approximately 40 % compared to the pre-LCD period in January. However, the accumulation mode particles increased by approximately 20 % as several polluted episodes contributed to secondary aerosol formation. In this study, new particle formation (NPF) events were found to be enhanced in the nucleation and growth processes during the LCD


Introduction
As a response to the outbreak of the 2019 novel coronavirus (COVID-19), the Chinese government implemented restrictions on population movement in February 2020; the period during which the restrictions were enforced was also called the lockdown (LCD) period.During the LCD period, the NO x emission was reduced by approximately 50 % in China, as retrieved by the satellite (Zhang et al., 2021) and ground-based measurements (Huang et al., 2021).The number concentration of Aitken mode particles (∼ 25-100 nm), which is related to the traffic emissions (Deventer et al., 2018), is also expected to decrease.The significant decrease in aerosol and precursor emissions during LCD is associated Published by Copernicus Publications on behalf of the European Geosciences Union.
with reduced human and economic activities.However, several heavy haze pollution periods occurred in the Yangtze River Delta (YRD) and the Beijing-Tianjin-Hebei (BTH) region.Secondary particles contributed significantly to air pollution, and NO x reduction favored increased ozone and atmospheric oxidizing capacity (Huang et al., 2021).The aerosol heterogeneous reaction process was also enhanced by the anomalously high humidity in northern China (Le et al., 2020).Furthermore, particle accumulation could also be favored by stagnant airflow and vertical meteorological conditions during LCD (Zhong et al., 2018).
New particle formation (NPF) has been an active global research topic for the last two decades because of its potential climatic implications (Kulmala et al., 2004).Nucleated particles can reach number concentrations of 10 4 -10 6 cm −3 .Subsequent growth contributes significantly to cloud condensation nuclei (CCN) (Kerminen et al., 2012) and can cause air pollution (Guo et al., 2014).Primary emissions of particulate matter (PM), CO, SO 2 , and NO 2 decreased significantly after the strict clear-air action plans were implemented in the last decade by the Beijing government (Zhang et al., 2019).Changes in SO 2 and background aerosols, the key factors influencing NPF events, are also linked to the formation (J ) and growth rate (GR) of secondary particles (Kyrö et al., 2014).Nanoparticles (diameter ≤ 100 nm) make minor particle mass contributions but pose a serious risk to human health because of high number concentrations and deep respiratory and cardiovascular system penetration (Kawanaka et al., 2009).However, the size-resolved, chemical, and toxicological properties of nanoparticles are unclear (Jin et al., 2017).Under unfavorable meteorological conditions, the growth of the nanoparticles for several consecutive days would even probably lead to particle mass enhancement as found in Beijing, China (Guo et al., 2014).
In a previous study, the influence of NPF event occurrence by emission reduction in Beijing was analyzed for China's Victory Day parade in August 2015 and for the summer Olympics in 2008; during this period, higher NPF occurrence frequency but lower J and GR was reported as a result of low precursor concentrations (Shen et al., 2016).In the present study, we focus on changes in particle number size distribution and NPF events during LCD in Beijing and the influencing factors.The link between NPF events and regional aerosol pollution is also explored.Our study will facilitate the optimization of regulatory measures to control particle and gas pollution in China, especially with regard to the variation of NPF-associated condensing vapors caused by reduced precursor emissions and elevated atmospheric oxidizing level.

Measurements
The particle and ion number size distribution measurements were conducted on the roof of the Chinese Academy of Meteorological Sciences (CAMS) building on the Chinese Meteorological Administration campus between January and February 2020.The site is approximately 53 m above ground level and located in the western Beijing urban area between the second and third ring roads.A major road with heavy traffic to the west of the site indicated that the sample air could be influenced by traffic emissions.More information about the site can be found in X. Wang et al. (2018).

Instrumentation
The number of particles of sizes 10-850 nm was measured using a scanning mobility particle sizer (SMPS, TROPOS, Germany).The system is a combination of a differential mobility analyzer (DMA) and a condensation particle counter (CPC, Model 3772, TSI Inc., USA).The mobility distribution of naturally charged and neutral nanoparticles is measured by a neutral cluster and air ion spectrometer (NAIS) with a 10 min time resolution (Mirme et al., 2007;Mirme and Mirme, 2013).The measured mobility was in the range 3.3-0.0013cm 2 V −1 s −1 , corresponding to mobility diameters of 0.8-42 nm.Positive and negative ions were simultaneously classified by two cylindrical DMAs and detected with 21 electrometers on the outer cylinder.A high sample flow rate of 60 L min −1 was used to minimize diffusion losses.In ion mode, the detected signal is inverted to a mobility distribution consisting of 28 bins, taking into account the measured background and experimentally determined diffusion losses.In neutral particle mode, the sample aerosol is charged using corona chargers, and the charged fraction is calculated (Fuchs, 1963).However, the lowest detection limit for the NAIS in the neutral particle mode (approximately 2 nm) was affected by the corona-generated ions (Asmi et al., 2009;Manninen et al., 2011).The lowest detection limit of the NAIS in ion mode was determined by the charging probability, nanoparticle concentration, and charger ion mobility (Kulmala et al., 2013).
Volatile organic compounds (VOCs) were measured using a proton-transfer-reaction time-of-flight mass spectrometer (PTR-ToF-MS 8000, IONICON) with a hydronium ion (H 3 O + ) source at CAMS site.About 30 kinds of compounds could be detected by the PTR-ToF-MS, by using the linear regression multipoint calibrations (Yuan et al., 2017).In this study, the mixing ratio of isoprene and major C6-C9 VOCs were derived with 1 h time resolution, as they are good indicators of anthropogenic VOC plumes (Dai et al., 2017).
The mass concentrations of PM 2.5 , precursor gases of O 3 , SO 2 , NO 2 , and CO at the GuanYuan air quality monitoring site were derived from the China National Environmen-tal Monitoring Center (CNEMC, http://www.cnemc.cn,last access: 5 May 2021), which is 3 km from the CAMS site.The global radiation at the observatory (54 511) in the southern Beijing urban area was used to estimate the sulfuric acid in this work.The solar radiation datasets were provided by the National Meteorological Information Center of the China Meteorological Administration.The meteorological factors used in this study -wind speed (WS), wind direction (WD), and relative humidity (RH) -were derived from the Haidian National Basic Meteorological Station (54399).The data can represent meteorological conditions at the CAMS site, which is located ∼ 5 km northwest of the urban area site.

NPF parameter calculation
The total particle and ion formation rate at 2 nm (J 2,tot and J 2,ion ) can be calculated from the particle and ion number concentrations in the size range 2-3 nm (Hirsikko et al., 2011;Manninen et al., 2010).J 2,tot and J 2,ion included time changes in the concentration of 2-3 nm particles or ions (first term on the right side of Eqs. 1 and 2), coagulation loss of 2-3 nm particles or ions with the pre-existing particles derived by SMPS (second term), and growth of 2-3 nm particles or ions into larger sizes by the GR (third term).In Eq. ( 2), the fourth and fifth terms represent loss due to ion-ion recombination and formation from ion-neutral attachment.The equations are given by the following formulas: N 2-3,tot and N ± 2-3,ion are the number concentration of particles and ions of positive and negative charges, respectively.CoagS 2 is the 2 nm coagulation coefficient.α and β (the ion-ion recombination and ion-neutral attachment coefficients, respectively) are assumed to be 1.6 × 10 −6 and 10 −8 cm 3 s −1 , respectively (Hoppel, 1985).
GR is defined as the rate of change of diameter with time, GR = (D p,2 − D p,1 )/dt, given in nm h −1 , where D p,1 and D p,2 are the geometric mean diameters (GMDs) when the nucleated particles start and stop growing, respectively.GMDs are derived by the log-normal modal fitting of the particle and ion number size distributions (Hussein et al., 2009).
Sulfuric acid (H 2 SO 4 ) is a key component in the nucleation process (Kulmala et al., 2013).The concentration of H 2 SO 4 was not measured directly in this study, and different proxy methods were used to derive the proxy sulfuric acid.One of these methods (Eq. 3) depends on the global radiation (Glob_R), SO 2 , and condensation sink (CS) and is developed according to the previous study conducted in a forest site, Hyytiälä, Finland (Petäjä et al., 2009).
where k is the empirically derived factor and well correlated with Glob_R (k = 1.4 × 10 −7 × Glob_R −0.7 , unit: m 2 W −1 s −1 ).The proxy equation is site-specific due to the different atmospheric conditions.In a polluted atmosphere, such as in Beijing, several proxy methods were also constructed based on a number of available atmospheric parameters (Lu et al., 2019).In this study, the simplest proxy (Eq.4) with the best performance (Eq.5) recommended by Lu et al. ( 2019) is adopted to derive the proxy sulfuric acid.
[H 2 SO 4 ] is the gaseous sulfuric acid with the unit of molecules cm −3 .[SO 2 ], [O 3 ], and [NO x ] are the concentrations of sulfur dioxide, ozone, and nitrogen oxides, with the unit of molecules cm −3 .UVB is the intensity of ultraviolet radiation b in W m −2 .CS is the condensation sink, which describes how fast the vapor molecules condense on the existing particles (Dal Maso et al., 2002), with the unit of s −1 .
The proxy method has been validated by comparing the measured sulfuric acid with a high correlation coefficient of 0.86 (Lu et al., 2019), based on the field campaign conducted approximately 2 km away from the CAMS site.Although the direct measurement of UVB was not available, it had been reported by Hu et al. (2013) that the monthly average of the ratio of UVB to global radiation (Glob_R) ranged from 0.007 % to 0.017 % in Beijing.And in this study, the average ratio of January and February (0.008 %) was applied to derive UVB by 0.008 % × Glob_R.The covariance of CS and SO 2 was found (correlation coefficient R = 0.83) that offset the dependence of sulfuric acid on CS by Lu et al. (2019).However, the anthropogenic emission sharply decreased during LCD in this study, and R was 0.45 for SO 2 and CS.To minimize the uncertainty of H 2 SO 4 proxy, the average value of three calculation methods was applied for the further analysis.

Typical NPF event identification
NPF events are identified and different nucleation types are characterized based on the daily evolution of particle number size distribution (PNSD).The burst of nucleation mode particles with diameter ≤ 25 nm appeared in the PNSD, and the burst should prevail over a few hours with clear growth process (Dal Maso et al., 2005).Regional NPF events can occur over a geographically large area and extend over several hundred kilometers (Shen et al., 2018).Such events indicate regional cases in which freshly nucleated particles can reach the size of CCN (Shen et al., 2011).(Draxler and Hess, 1998;Wang et al., 2009).

The meteorological conditions
The meteorological parameters during the LCD period, January and February 2020, as well as the average conditions of January and February 2016-2020 were analyzed and the diurnal pattern was given (Fig. 1).It showed much higher RH, lower WS, slightly higher T , and lower pressure during LCD (January and February 2020) than that of 5-year climatology average condition (January and February 2016-2020).The anomaly of monthly mean sea level pressure in January and February between 2020 and 2016-2020 was analyzed based on the ECMWF reanalysis dataset (ERA5, https://cds.climate.copernicus.eu/,last access: 6 May 2021), as given in the Supplement (Fig. S1).It showed a negative anomaly in the BTH region, indicating the air pressure decreased in January and February 2020, as compared with the corresponding period of the 5-year climatology.The local air convergence resulted in high RH and low WS, which favored the air pollutants accumulating (Zhong et al., 2018).The unfavorable meteorological trapped moisture and pollutants near the ground could thus offset substantial emissions reductions during COVID-19 LCD to some extent.

Overview of the NSD of particles and charged ions
Figure 2 shows the time evolution of the number size distribution (NSD) of particles in the 10-850 nm range, neutral particles (2-42 nm), and charged ions (0.8-42 nm) in January and February 2020.The dataset was classified into the COVID-19 LCD (24 January-16 February 2020), pre-LCD period (3-23 January 2020), and post-LCD (17-29 February 2020) periods to reveal the influence of emission reductions.The NPF event occurred on 10 out of 23 d during pre-LCD, 10 out of 24 d in LCD, and 5 out of 13 d in post-LCD, respectively.Poisson statistics was conducted for NPF event occurrence probability for pre-LCD, LCD, and post-LCD periods as given in Fig. S2 in the Supplement.It showed slight variation of NPF event occurrence probability, as compared with pre-LCD and LCD periods.Despite the large primary emissions reduction, several cases of heavy aerosol pollu-tion events occurred in the BTH region during LCD.Particle matter below 2.5 µm (PM 2.5 ) mass concentration at air monitoring sites in Beijing at the Ministry of Ecology and Environment of China exceeded 75 µg m −3 (the second grade of the Ambient Air Quality Standard of China) on 12 of the 28 d, which were identified as polluted conditions.The elevated PM mass concentration was attributed to the secondary aerosol formation process; this process was aided by the enhanced oxidizing capacity caused by increased ozone levels (Huang et al., 2021).
The particle number concentrations of the Aitken mode (25-100 nm, N 25-100 nm ) and the accumulation mode (100-850 nm, N 100-850 nm ) derived by SMPS and the nucleation mode (≤ 25 nm) of neutral particles and charged ions by NAIS were given in Fig. 3 and discussed in detail in the following.The Aitken mode showed a significant reduction since the Chinese New Year (24 January) and normal fluctuations below 3000 cm −3 during LCD and post-LCD.Mean N 25-100 concentrations were 4040±1590, 2400±1170, and 2170 ± 994 cm −3 during pre-LCD, LCD, and post-LCD, respectively.Aitken mode particles were closely related to the anthropogenic emissions and reduced by approximately 40 %.During post-LCD, the Aitken mode concentration remained low because people were encouraged to work at home and services were almost shut down.Accumulation mode particles usually undergo coagulation, condensation, heterogeneous reactions, and long-range transport processes that can reflect regional polluted conditions.N 100-850 nm concentrations were 1820 ± 1190, 2200 ± 1320, and 1850 ± 840 cm −3 during pre-LCD, LCD, and post-LCD, respectively; the 20 % increase during LCD (compared with pre-LCD) occurred despite large emissions reductions and was related to specific pollution episodes that occurred from 24-26 January and 12-14 February.The particle number concentration derived from SMPS is probably lower than that from NAIS in the overlap size range of 20-40 nm, because the overestimation of natural particle concentration as a multiple charge effect above 20 nm is beyond the instrumental detection limit (Gagné et al., 2011).In this study, the number concentration of 20-40 nm was integrated by the SMPS and NAIS particle mode (N 20-40 nm,smps and N 20-40 nm,nais ) with an enhancement factor (N 20-40 nm,nais /N 20-40 nm,smps ) of 1.65 ± 0.06, and the number concentration of particles larger than 20 nm derived by SMPS was more accurate.

NPF event variation
Table 1 provides the key parameters describing NPF events, including NPF days and available measurement days, CS, J 2 , and GR for total particles and charged ions.Higher J 2 and GR values for particles and ions were also found during LCD and post-LCD than during pre-LCD.However, the emissions control period during the China Victory Day Parade in Beijing in 2015 (20 August-3 September) featured higher frequency and decreasing J 3 and GR trends compared with the corresponding month in 2010-2013 (Shen et al., 2016).J 3 represented the formation rate at 3 nm calculated from the particle number concentration of 3-4 nm particles by Eq. ( 1), as the lowest detection limit of SMPS applied in 2015 and the 2010-2013 campaign was 3 nm.That indicated the factors influencing the NPF event, including precursors, preexisting particles, and meteorological conditions, were complex and should be evaluated further.The daily mean value of NO 2 decreased by ∼ 35 % and SO 2 decreased by ∼ 13 %, whereas O 3 increased by 80 % during LCD as compared to pre-LCD in this work (Fig. 4).The probability density function (PDF) was analyzed for hourly SO 2 , NO 2 , and O 3 during pre-LCD, LCD, and post-LCD, respectively, and the result was given in the Supplement (Fig. S3).It also showed a significant decreasing trend of NO 2 but an increasing trend of O 3 as compared with pre-LCD and LCD / post-LCD.However, the variation of SO 2 among different periods was not clear, as the SO 2 concentration remained low due to the emission control in these years.Previous studies had indicated that NO x suppressed NPF events by influencing the formation of highly oxidized VOCs, which participated in nucleation and initial particle growth (Lehtipalo et al., 2018;Yan et al., 2016Yan et al., , 2020)), suggesting that the reduction of NO 2 during LCD provided favorable conditions for particle growth.
In this work, five kinds of VOCs (isoprene, benzene, toluene, and C8 and C9 aromatics) are discussed, which are the indicators of anthropogenic VOC and also could be oxidized to contribute to the growth process (Dai et al., 2017).The result (Fig. 5) showed C8 and C9 aromatics decreased by approximately 20 % and 8 % during the LCD as compared with pre-LCD; however, isoprene and toluene slightly changed, benzene increased by approximately 21 % during LCD period.It also suggested the VOCs we focused on did not show the reduction rate as 45 % as Huang et al. (2021) reported in the BTH region.The major oxidized VOCs formation pathways are the oxidation by O 3 , OH, and NO 3 radicals (Ehn et al., 2012).As mentioned above, O 3 increased by 80 % during the LCD period.We used Glob_R as a simple proxy of OH, and Glob_R increased by ∼ 24 % during LCD as compared with pre-LCD, as given in the Supplement (Fig. S4).NO 3 oxidation of nocturnal biogenic VOCs is also an important pathway of secondary organic aerosol formation in Beijing (H.Wang et al., 2018).NO 3 is predominantly formed by the reaction of NO   1. Parameters characterizing NPF events during pre-LCD, LCD, and post-LCD, including NPF frequency, formation rate (J 2,par , J 2,pos_ion , J 2,neg_ion ), and growth rate (GR 2,par , GR pos_ion , GR neg_ion ) of the total particles and charge ions, as well as condensation sink (CS).
Pre-LCD LCD Post-LCD NPF event (available days) 10 ( 23) 10 ( 24) 5 (13) J 2,par (cm −3 s −1 ) 5.6 ± 2.3 7.9 ± 4.5 5.9 ± 3.5 J 2,pos_ion (cm −3 s −1 ) 0.010 ± 0.003 0.032 ± 0.003 0.021 ± 0.014 J 2,neg_ion (cm −3 s −1 ) 0.009 ± 0.004 0.024 ± 0.005 0.015 ± 0.011 GR par (nm h −1 ) 0.8 ± 0.5 1.5 ± 0.7 2.0 ± 0.5 GR pos_ion (nm h −1 ) 1.8 ± 0.3 3.1 ± 0.2 3.6 ± 0.4 GR neg_ion (nm h −1 ) 2.0 ± 0.7 3.1 ± 0.4 3.2 ± 0.4 CS (s −1 ) 0.010 ± 0.003 0.008 ± 0.006 0.08 ± 0.003 it showed the variations of precursors, solar radiation, and CS could finally influence NPF by photochemical reactions with VOCs and sulfuric acid production, promoting the nucleation and growth process.The H 2 SO 4 proxy were derived according to Eqs. ( 3)-( 5) as given in Fig. 6, and the mean value of the three methods was discussed.For LCD and pre-LCD during the NPF event occurrence (09:00-16:00 LT), CS decreased by ∼ 25 % and Glob_R increased by ∼ 40 %, whereas SO 2 decreased by ∼ 28 %.The variations of these variables finally lead to a H 2 SO 4 increase of ∼ 26 %.The formation of sulfuric acid was aided by the enhanced atmospheric oxidizing capacity because of elevated O 3 concentration during LCD, which had also been validated in the previous study in Nanjing, YRD, China (Huang et al., 2021).The H 2 SO 4 proxy was correlated with J 2,tot and GR, with the R value of 0.62 for J 2,tot and the H 2 SO 4 , and 0.45 for GR and the H 2 SO 4 , re-spectively.Based on the NAIS data of the neutral particle mode, the hourly mean geometric mean diameter of the nucleation mode (D p,nuc ) was fitted to show the growth process and its relationship with proxy H 2 SO 4 (Fig. 7).It also revealed that in the initial growth process (D p,nuc < 5 nm), D p,nuc increased positively with the H 2 SO 4 proxy.Furthermore, GR in the size range of 3-5 nm was slightly higher during LCD and post-LCD, as compared with pre-LCD, indicating the enhanced effect of sulfuric acid on the initial growth of the nucleated particles.However, when the nucleated particles grew into the larger sizes (> 5 nm), the H 2 SO 4 proxy decreased, which is probably related to the weak solar radiation in late afternoon and could not explain the continuous growth, and the oxidized VOCs could be the main contributor.The non-linear dependence of J 2,tot and GR on the condensing vapors indicates a complex mechanism in the multi-component nucleation and growth system.et al. ( 2020) revealed that sulfuric acid played an important role in smaller growth processes from 2-10 nm; however, they could not explain condensational growth when the nucleated particles overcame 10 nm.For particles larger than 10 nm, low volatile organic vapors should contribute to growth (Kontkanen et al., 2018;Yan et al., 2020).

Effect of charged ions
Table 1 provided the parameters describing the nucleation and growth process for neutral particles and positive and negative ions, which showed that the GR of ions was larger than that of neutral particles.Growth enhancement from charge-dipole interactions between condensable gases and charged ions lead to higher growth rates than with neutral particles (Nadykto and Yu, 2003;Yu and Turco, 2000).The growth process of D p,nuc of neutral particles and positive ions were given in Fig. 8.It showed D p,nuc,ion grow faster than D p,nuc,par , especially for the sizes below 5 nm, depending on the growth rate in each time interval ((D p,nuc,t1 − D p,nuc,t2 )/ t, t = 1 h).The enhanced growth rate factor (GR p,nuc,ion /GR p,nuc,par ) ranged from 1.1 to 1.7, with the average of 1.38 ± 0.34 during the entire particle growth process and higher (∼ 2.0) for the initial size of 2-5 nm.The growth of the nano-sized particles was not linear (especially at the initial size); therefore, the GR calculation was split into different size ranges (Fig. 9).The GR of charged ions was higher than that of neutral particles for all size ranges, which is consistent with previous studies (Hirsikko et al., 2005;Suni et al., 2008), and the difference was much larger at initial sizes below 5 nm as indicated above.In addition to condensational growth, the difference in the loss rates of smaller particles (neutral, positive, negative) due to the coagulation process and ion-ion recombination also affects particle size and calculated GRs (Yu andTurco, 2008, 2011).The effect of the charge decreases as particle size increases, and more species condense as particles grow.However, the number concentration of charged ions plays a minor role in the total particle count, and their contribution to the total growth process and nucleation can be ignored in urban Beijing, where the nucleation mechanism is dominated by neutral pathways with abundant condensing vapors.

Air pollution episode followed by NPF event
In this study, two severe pollution episodes occurred during LCD from 24-29 January and 7-14 February, with daily average PM 2.5 mass concentrations in the range 75-  mass change and planetary boundary layer (PBL) development (Wiedensohler et al., 2009).The back trajectories arriving at CAMS station at 12:00 LT from 4 to 14 February with the terminal height of 500 m a.g.l. were calculated (Fig. 11).The result showed back trajectories originating from the northwest from 4 to 10 February, corresponding to the dry and clean air masses.However, from 11 to 13 February, the southwesterly air masses were dominant and favored the accumulating of the particles, resulting in the high concentration level of PM 2.5 .In the first stage (5-10 February), the secondary aerosol formation was the key process contributing to increasing PM 2.5 mass.The continuous growth of nucleated particles was sometimes interrupted by the development of PBL and local wind.As in the second stage (11-13 February), PM 2.5 reached a peak value of 250 µg m −3 , and PM 2.5 / CO slightly decreased with small fluctuations.Because primary emission should not change during this period, the unfavorable meteorological conditions could be responsible for the event.Low WS and high RH (from 80 % to > 90 %) was found from 5-14 February, with a few hours of RH < 60 % during the daytime.Particle hygroscopic growth under high-ambient-RH conditions and heterogeneous reactions on particle surfaces could also contribute to the elevated particle mass concentration (X.Wang et al., 2018).Consequently, nucleated particles accumulated because of enhanced oxidizing capacity and unfavorable meteorological conditions, causing the severe aerosol pollution.

Conclusion
In this study we presented changes in the NSD of particles and charged ions measured between January and Febru-ary 2020.These observations reveal the influence of emission reduction on NPF events.Particles smaller than 100 nm were effectively reduced by ∼ 40 % because of suspended human activities during the Chinese New Year and the COVID-19 LCD.The accumulation mode particles were slightly higher during LCD, as several hazy days were associated with secondary aerosol formation.The frequency of NPF days slightly varied; however, J 2 and GR were significantly higher.During LCD, NO x , and SO 2 concentrations decreased as anthropogenic emissions decreased.Higher O 3 and a lower condensation sink raised sulfuric acid concentration levels by ∼ 26 %, which were responsible for the higher nucleation rate and larger nanoparticle quantity.Sulfuric acid was also responsible for the nucleated particle growth at the initial sizes (below 5 nm).In the late afternoon, sulfuric acid decreased as the weakened solar radiation and low-volatility oxidation products of VOCs could have larger contribution to the particle growth.For the major VOCs, isoprene and toluene were slightly changed, benzene increased, and aromatics (C8 and C9 compounds) decreased during the LCD period.Although the oxidation products of VOCs were not measured in this study, the major oxidants of VOCs (O 3 , OH, and NO 3 ) all increased during LCD period, indicating the possibility of enhanced oxidized VOCs promoting the particle growth process.The effect of charged ions on the particle growth was also studied and it showed an enhanced growth rate factor of 1.38 ± 0.34.The nucleated particles entered accumulation mode by secondary aerosol formation and underwent hygroscopic growth under high RH and calm wind conditions, which facilitated the occurrence of severe pollution episodes during LCD.This work highlights the potential influence of strict emission control strategies on NPF events and provides insights into the positive and negative effects of precursors and atmospheric oxidizing capacity on the nucleation and growth process of the nanoparticles.

Figure 1 .
Figure 1.The mean diurnal pattern of meteorological parameters, including temperature (a), RH (b), sea level pressure (c), and wind speed (d) during the LCD period (24 January-16 February 2020), January and February 2020, and January and February 2016-2020.The solid circles and bars represent the mean value and the standard deviation, respectively.

Figure 2 .
Figure 2. Time evolution of number size distribution of 10-850 nm particles by SMPS (a), neutral 2-42 nm particles by NAIS in positive particle mode (b), and positive 0.8-42 nm ions by NAIS (c).NPF events were marked by numbers from 1-25.

Figure 3 .
Figure 3.Time series of hourly mean of the number concentrations for different size ranges, including 25-100 and 100-850 nm from SMPS data (a), 2-10 nm particles from NAIS and 10-25 nm particles from both NAIS and SMPS (b), and 1-10 nm and 10-25 nm positive ions from NAIS (c).

Figure 4 .
Figure 4. Concentration level of PM 2.5 mass concentration (a) and precursors (b), including NO 2 , SO 2 , and O 3 during the measurement period.The circle and bar indicate the mean and standard deviation, respectively; NPF days are marked with continuous numbers 1-25.

Figure 5 .
Figure 5.Time series of isoprene, benzene, toluene, and C8 and C9 aromatics (a-e) during 5 January to 15 February, and the probability distribution function of mixing ration of each VOC component (f-j), respectively.

Figure 6 .
Figure 6.The sulfuric acid concentrations derived by different proxy equations.The red and orange lines indicate the result of the N2 and N7 methods by Lu et al. (2019), and the blue line indicates the calculation result based on the method recommended by Petäjä et al. (2009).

Figure 7 .
Figure 7. Scatter plot between geometric mean diameter of nucleation mode (D p,nuc ) and the proxy sulfuric acid.The grey dots and crosses represent the NPF events during pre-LCD and LCD / post-LCD, respectively.The purple and blue lines represent the mean conditions during pre-LCD, LCD / post-LCD.The vertical and horizontal bars represents the standard deviations of sulfuric acid and D p,nuc .

Figure 8 .
Figure 8.The time evolution of geometric mean diameter of nucleation mode (D p,nuc ) of neutral particle and positive charged ions during the NPF events.The circle and bar present the mean value and the standard deviation.

Figure 11 .
Figure 11.The back trajectories arriving at CAMS station at 12:00 LT form 4 to 14 February with the terminal height of 500 m a.g.l.