363 citations as recorded by crossref.

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18. Highly Hygroscopic Aerosols Facilitate Summer and Early‐Autumn Cloud Formation at Extremely Low Concentrations Over the Central Arctic Ocean P. Duplessis et al. 10.1029/2023JD039159
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25. Size-resolved cloud condensation nuclei (CCN) activity and closure analysis at the HKUST Supersite in Hong Kong J. Meng et al. 10.5194/acp-14-10267-2014
26. New particle formation and its CCN enhancement in the Yangtze River Delta under the control of continental and marine air masses X. Fang et al. 10.1016/j.atmosenv.2021.118400
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30. CCN closure study: Effects of aerosol chemical composition and mixing state D. Bhattu & S. Tripathi 10.1002/2014JD021978
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36. Size-resolved CCN distributions and activation kinetics of aged continental and marine aerosol A. Bougiatioti et al. 10.5194/acp-11-8791-2011
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46. Cloud condensation nuclei over the Bay of Bengal during the Indian summer monsoon D. Chate et al. 10.1007/s00376-017-6331-z
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48. Connecting hygroscopic growth at high humidities to cloud activation for different particle types H. Wex et al. 10.1088/1748-9326/3/3/035004
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50. Characterization of aerosol properties at Cyprus, focusing on cloud condensation nuclei and ice-nucleating particles X. Gong et al. 10.5194/acp-19-10883-2019
51. Aitken mode particles as CCN in aerosol- and updraft-sensitive regimes of cloud droplet formation M. Pöhlker et al. 10.5194/acp-21-11723-2021
52. Role of Sea Surface Microlayer Properties in Cloud Formation B. Hendrickson et al. 10.3389/fmars.2020.596225
53. Soluble mass, hygroscopic growth, and droplet activation of coated soot particles during LACIS Experiment in November (LExNo) S. Henning et al. 10.1029/2009JD012626
54. Direct Comparison of the Submicron Aerosol Hygroscopicity of Water-Soluble Sugars J. Dawson et al. 10.1021/acsearthspacechem.0c00159
55. Respiratory aerosols and droplets in the transmission of infectious diseases M. Pöhlker et al. 10.1103/RevModPhys.95.045001
56. Size distribution and chemical composition of primary particles emitted during open biomass burning processes: Impacts on cloud condensation nuclei activation L. Chen et al. 10.1016/j.scitotenv.2019.03.419
57. The influence of chemical composition and mixing state of Los Angeles urban aerosol on CCN number and cloud properties M. Cubison et al. 10.5194/acp-8-5649-2008
58. Aerosol Chemistry Resolved by Mass Spectrometry: Linking Field Measurements of Cloud Condensation Nuclei Activity to Organic Aerosol Composition A. Vogel et al. 10.1021/acs.est.6b01675
59. Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation E. Mikhailov et al. 10.5194/acp-21-6999-2021
60. CCN Data Interpretation Under Dynamic Operation Conditions T. Raatikainen et al. 10.1080/02786826.2014.899429
61. Cloud condensation nuclei in polluted air and biomass burning smoke near the mega-city Guangzhou, China – Part 2: Size-resolved aerosol chemical composition, diurnal cycles, and externally mixed weakly CCN-active soot particles D. Rose et al. 10.5194/acp-11-2817-2011
62. Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition J. Schmale et al. 10.1038/sdata.2017.3
63. Influence of gas-to-particle partitioning on the hygroscopic and droplet activation behaviour of α-pinene secondary organic aerosol Z. Jurányi et al. 10.1039/b904162a
64. Aerosol–Cloud Interaction at the Summit of Mt. Fuji, Japan: Factors Influencing Cloud Droplet Number Concentrations Y. Iwamoto et al. 10.3390/app11188439
65. Global organic and inorganic aerosol hygroscopicity and its effect on radiative forcing M. Pöhlker et al. 10.1038/s41467-023-41695-8
66. Towards closing the gap between hygroscopic growth and activation for secondary organic aerosol – Part 2: Theoretical approaches M. Petters et al. 10.5194/acp-9-3999-2009
67. The Role of Temperature in Cloud Droplet Activation S. Christensen & M. Petters 10.1021/jp3064454
68. The impact of aerosol size-dependent hygroscopicity and mixing state on the cloud condensation nuclei potential over the north-east Atlantic W. Xu et al. 10.5194/acp-21-8655-2021
69. Chemical aging of single and multicomponent biomass burning aerosol surrogate particles by OH: implications for cloud condensation nucleus activity J. Slade et al. 10.5194/acp-15-10183-2015
70. Hygroscopic properties and cloud condensation nuclei activity of atmospheric aerosols under the influences of Asian continental outflow and new particle formation at a coastal site in eastern Asia H. Cheung et al. 10.5194/acp-20-5911-2020
71. In-situ observations reveal weak hygroscopicity in the Southern Tibetan Plateau: implications for aerosol activation and indirect effects Y. Wang et al. 10.1038/s41612-024-00629-x
72. From Water Clustering to Osmotic Coefficients M. Frosch et al. 10.1021/jp103129u
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76. Development of a cloud condensation nuclei (CCN) counter using a laser and charge-coupled device (CCD) camera M. Park et al. 10.1007/s11783-011-0346-y
77. Cloud activation properties of aerosol particles in a continental Central European urban environment I. Salma et al. 10.5194/acp-21-11289-2021
78. Reconsideration of surface tension and phase state effects on cloud condensation nuclei activity based on the atomic force microscopy measurement C. Xiong et al. 10.5194/acp-22-16123-2022
79. Scanning Flow CCN Analysis—A Method for Fast Measurements of CCN Spectra R. Moore & A. Nenes 10.1080/02786820903289780
80. Reconciliation of measurements of hygroscopic growth and critical supersaturation of aerosol particles in central Germany M. Irwin et al. 10.5194/acp-10-11737-2010
81. Wetting properties of fresh urban soot particles: Evaluation based on critical supersaturation and observation of surface trace materials S. Ueda et al. 10.1016/j.scitotenv.2021.152274
82. A broad supersaturation scanning (BS2) approach for rapid measurement of aerosol particle hygroscopicity and cloud condensation nuclei activity H. Su et al. 10.5194/amt-9-5183-2016
83. Comprehensive Simultaneous Shipboard and Airborne Characterization of Exhaust from a Modern Container Ship at Sea S. Murphy et al. 10.1021/es802413j
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98. Using Raman Microspectroscopy to Determine Chemical Composition and Mixing State of Airborne Marine Aerosols over the Pacific Ocean C. Deng et al. 10.1080/02786826.2013.867297
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181. African smoke particles act as cloud condensation nuclei in the wintertime tropical North Atlantic boundary layer over Barbados H. Royer et al. 10.5194/acp-23-981-2023
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184. Cloud droplet activation of mixed organic-sulfate particles produced by the photooxidation of isoprene S. King et al. 10.5194/acp-10-3953-2010
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188. The Effect of Relative Humidity on Continental Average Aerosols B. Tijjani et al. 10.4236/ojapps.2014.47038
189. Gas–particle interactions of tropospheric aerosols: Kinetic and thermodynamic perspectives of multiphase chemical reactions, amorphous organic substances, and the activation of cloud condensation nuclei U. Pöschl 10.1016/j.atmosres.2010.12.018
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191. Condensation/immersion mode ice-nucleating particles in a boreal environment M. Paramonov et al. 10.5194/acp-20-6687-2020
192. Femtosecond filamentation induced particles and their cloud condensation nuclei activity L. Ran et al. 10.1016/j.atmosenv.2019.03.019
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194. CCN Spectra, Hygroscopicity, and Droplet Activation Kinetics of Secondary Organic Aerosol Resulting from the 2010 Deepwater Horizon Oil Spill R. Moore et al. 10.1021/es203362w
195. The NPF Effect on CCN Number Concentrations: A Review and Re‐Evaluation of Observations From 35 Sites Worldwide J. Ren et al. 10.1029/2021GL095190
196. Why would apparent κ linearly change with O/C? Assessing the role of volatility, solubility, and surface activity of organic aerosols S. Nakao 10.1080/02786826.2017.1352082
197. A study on aerosol-cloud condensation nuclei (CCN) activation over eastern Himalaya in India A. Roy et al. 10.1016/j.atmosres.2017.01.015
198. Airborne and ground based CCN spectral characteristics: Inferences from CAIPEEX – 2011 M. Varghese et al. 10.1016/j.atmosenv.2015.06.041
199. Effect of chemical mixing state on the hygroscopicity and cloud nucleation properties of calcium mineral dust particles R. Sullivan et al. 10.5194/acp-9-3303-2009
200. What controls volatility of sea spray aerosol? Results from laboratory studies using artificial and real seawater samples B. Rasmussen et al. 10.1016/j.jaerosci.2017.02.002
201. The importance of aerosol mixing state and size-resolved composition on CCN concentration and the variation of the importance with atmospheric aging of aerosols J. Wang et al. 10.5194/acp-10-7267-2010
202. Thermochemical, Cloud Condensation Nucleation Ability, and Optical Properties of Alkyl Aminium Sulfate Aerosols A. Lavi et al. 10.1021/jp403180s
203. Size-resolved measurement of the mixing state of soot in the megacity Beijing, China: diurnal cycle, aging and parameterization Y. Cheng et al. 10.5194/acp-12-4477-2012
204. CCN activity of organic aerosols observed downwind of urban emissions during CARES F. Mei et al. 10.5194/acp-13-12155-2013
205. The occurrence of lower-than-expected bulk NCCN values over the marginal seas of China - Implications for competitive activation of marine aerosols J. Gong et al. 10.1016/j.scitotenv.2022.159938
206. Will Aerosol Hygroscopicity Change with Biodiesel, Renewable Diesel Fuels and Emission Control Technologies? D. Vu et al. 10.1021/acs.est.6b03908
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210. Impacts of organic aerosols and its oxidation level on CCN activity from measurement at a suburban site in China F. Zhang et al. 10.5194/acp-16-5413-2016
211. High-resolution physicochemical dataset of atmospheric aerosols over the Tibetan Plateau and its surroundings J. Xu et al. 10.5194/essd-16-1875-2024
212. Cloud condensation nuclei activity and hygroscopicity of fresh and aged cooking organic aerosol Y. Li et al. 10.1016/j.atmosenv.2017.11.035
213. CCN closure results from Indian Continental Tropical Convergence Zone (CTCZ) aircraft experiment M. Srivastava et al. 10.1016/j.atmosres.2013.05.025
214. Hygroscopic growth and cloud forming potential of Arctic aerosol based on observed chemical and physical characteristics (a 1 year study 2007–2008) S. Silvergren et al. 10.1002/2014JD021657
215. Investigating Primary Marine Aerosol Properties: CCN Activity of Sea Salt and Mixed Inorganic–Organic Particles S. King et al. 10.1021/es300574u
216. Relaxed step functions for evaluation of CCN counter data on size-separated aerosol particles B. Svenningsson & M. Bilde 10.1016/j.jaerosci.2008.03.004
217. Cloud condensation nuclei activity of isoprene secondary organic aerosol G. Engelhart et al. 10.1029/2010JD014706
218. Hygroscopic properties and cloud condensation nuclei activation of limonene-derived organosulfates and their mixtures with ammonium sulfate A. Hansen et al. 10.5194/acp-15-14071-2015
219. Atmospheric aerosol properties at a semi-rural location in southern India: particle size distributions and implications for cloud droplet formation S. Shika et al. 10.1007/s42452-020-2804-2
220. Assessment of cloud condensation nucleus activation of urban aerosol particles with different hygroscopicity and the application to the cloud parcel model K. Kawana et al. 10.1002/2013JD020827
221. Prediction of size-resolved number concentration of cloud condensation nuclei and long-term measurements of their activation characteristics H. Che et al. 10.1038/s41598-017-05998-3
222. Cloud condensation nuclei measurements in the marine boundary layer of the Eastern Mediterranean: CCN closure and droplet growth kinetics A. Bougiatioti et al. 10.5194/acp-9-7053-2009
223. A 17 month climatology of the cloud condensation nuclei number concentration at the high alpine site Jungfraujoch Z. Jurányi et al. 10.1029/2010JD015199
224. Distribution and origin of aerosol and its transform relationship with CCN derived from the spring multi-aircraft measurements of Beijing Cloud Experiment (BCE) G. Lu & X. Guo 10.1007/s11434-012-5136-9
225. Variability of aerosol-cloud interactions induced by different cloud droplet nucleation schemes D. Chang et al. 10.1016/j.atmosres.2020.105367
226. Potential contribution of new particle formation to cloud condensation nuclei in Beijing D. Yue et al. 10.1016/j.atmosenv.2011.07.037
227. Cloud condensation nuclei activity and droplet formation of primary and secondary organic aerosol mixtures E. Fofie et al. 10.1080/02786826.2017.1392480
228. Variations in <i>N</i><sub>cn</sub> and <i>N</i><sub>ccn</sub> over marginal seas in China related to marine traffic emissions, new particle formation and aerosol aging Y. Gao et al. 10.5194/acp-20-9665-2020
229. Variation of CCN activity during new particle formation events in the North China Plain N. Ma et al. 10.5194/acp-16-8593-2016
230. Large contribution of organics to condensational growth and formation of cloud condensation nuclei (CCN) in the remote marine boundary layer G. Zheng et al. 10.5194/acp-20-12515-2020
231. Consistency between parameterisations of aerosol hygroscopicity and CCN activity during the RHaMBLe discovery cruise N. Good et al. 10.5194/acp-10-3189-2010
232. Mathematical derivation and physical interpretation of particle size-resolved activation ratio based on particle hygroscopicity distribution: Application on global characterization of CCN activity X. Jiang et al. 10.1016/j.atmosenv.2020.118137
233. Characterization of aerosol chemical composition from urban pollution in Brazil and its possible impacts on the aerosol hygroscopicity and size distribution G. Almeida et al. 10.1016/j.atmosenv.2019.01.024
234. Scanning supersaturation condensation particle counter applied as a nano-CCN counter for size-resolved analysis of the hygroscopicity and chemical composition of nanoparticles Z. Wang et al. 10.5194/amt-8-2161-2015
235. Characterization and parameterization of aerosol cloud condensation nuclei activation under different pollution conditions H. Che et al. 10.1038/srep24497
236. Fog–Haze Transition and Drivers in the Coastal Region of the Yangtze River Delta R. Lyu et al. 10.3390/ijerph19159608
237. Numerical simulation on the effects of flow parameters on the detection performance of a self-developed condensation particle counter H. Guo et al. 10.1007/s11051-023-05865-5
238. Cloud condensation nuclei activity of fresh primary and aged biomass burning aerosol G. Engelhart et al. 10.5194/acp-12-7285-2012
239. Aircraft measurements of the vertical distribution and activation property of aerosol particles over the Loess Plateau in China J. Li et al. 10.1016/j.atmosres.2014.12.004
240. Surfactant effect on cloud condensation nuclei for two‐component internally mixed aerosols S. Petters & M. Petters 10.1002/2015JD024090
241. Gas-phase kinetics modifies the CCN activity of a biogenic SOA A. Vizenor & A. Asa-Awuku 10.1039/C8CP00075A
242. Reconciling atmospheric water uptake by hydrate forming salts B. Rosati et al. 10.1039/D0EM00179A
243. Measurement report: Cloud condensation nuclei activity and its variation with organic oxidation level and volatility observed during an aerosol life cycle intensive operational period (ALC-IOP) F. Mei et al. 10.5194/acp-21-13019-2021
244. Cloud condensation nuclei activity, closure, and droplet growth kinetics of Houston aerosol during the Gulf of Mexico Atmospheric Composition and Climate Study (GoMACCS) S. Lance et al. 10.1029/2008JD011699
245. Primary marine aerosol physical flux and chemical composition during a nutrient enrichment experiment in mesocosms in the Mediterranean Sea A. Schwier et al. 10.5194/acp-17-14645-2017
246. The Effect of Relative Humidity on Maritime Tropical Aerosols B. Tijjani et al. 10.4236/ojapps.2014.46029
247. On the competition among aerosol number, size and composition in predicting CCN variability: a multi-annual field study in an urbanized desert E. Crosbie et al. 10.5194/acp-15-6943-2015
248. Sensitivities of Amazonian clouds to aerosols and updraft speed M. Cecchini et al. 10.5194/acp-17-10037-2017
249. Integrating Cloud Condensation Nuclei Predictions with Fast Time Resolved Aerosol Instrumentation to Determine the Hygroscopic Properties of Emissions Over Transient Drive Cycles D. Vu et al. 10.1080/02786826.2015.1105358
250. Long-range transported North American wildfire aerosols observed in marine boundary layer of eastern North Atlantic G. Zheng et al. 10.1016/j.envint.2020.105680
251. Effect of organic compounds on cloud condensation nuclei (CCN) activity of sea spray aerosol produced by bubble bursting M. Moore et al. 10.1016/j.atmosenv.2011.04.034
252. Formation Mechanism of Atmospheric Ammonium Bisulfate: Hydrogen‐Bond‐Promoted Nearly Barrierless Reactions of SO3 with NH3 and H2O S. Chen et al. 10.1002/cphc.201701333
253. Cloud Condensation Nuclei and Immersion Freezing Abilities of Al₂O₃ and Fe₂O₃ Particles Measured with the Meteorological Research Institute's Cloud Simulation Chamber T. KUO et al. 10.2151/jmsj.2019-032
254. Correlation between cloud condensation nuclei concentration and aerosol optical thickness in remote and polluted regions M. Andreae 10.5194/acp-9-543-2009
255. Atmospheric Radiation Measurement (ARM) Aerosol Observing Systems (AOS) for Surface-Based In Situ Atmospheric Aerosol and Trace Gas Measurements J. Uin et al. 10.1175/JTECH-D-19-0077.1
256. Cloud droplet activity changes of soot aerosol upon smog chamber ageing C. Wittbom et al. 10.5194/acp-14-9831-2014
257. Impacts of methanesulfonate on the cloud condensation nucleation activity of sea salt aerosol M. Tang et al. 10.1016/j.atmosenv.2018.12.034
258. Water uptake by biomass burning aerosol at sub- and supersaturated conditions: closure studies and implications for the role of organics U. Dusek et al. 10.5194/acp-11-9519-2011
259. Droplet activation, separation, and compositional analysis: laboratory studies and atmospheric measurements N. Hiranuma et al. 10.5194/amt-4-2333-2011
260. Accurate representations of the physicochemical properties of atmospheric aerosols: when are laboratory measurements of value? A. Marsh et al. 10.1039/C7FD00008A
261. Using stable isotopes to trace sources and formation processes of sulfate aerosols from Beijing, China X. Han et al. 10.1038/srep29958
262. Cloud condensation nuclei (CCN) activity and oxygen-to-carbon elemental ratios following thermodenuder treatment of organic particles grown by α-pinene ozonolysis M. Kuwata et al. 10.1039/c1cp20253g
263. Hygroscopicity, CCN and volatility properties of submicron atmospheric aerosol in a boreal forest environment during the summer of 2010 J. Hong et al. 10.5194/acp-14-4733-2014
264. Dynamics of aerosol, humidity, and clouds in air masses travelling over Fennoscandian boreal forests M. Räty et al. 10.5194/acp-23-3779-2023
265. Assessment of cloud supersaturation by size-resolved aerosol particle and cloud condensation nuclei (CCN) measurements M. Krüger et al. 10.5194/amt-7-2615-2014
266. Characteristics of Scanning Flow Condensation Particle Counter (SFCPC): A rapid approach for retrieving hygroscopicity and chemical composition of sub-10 nm aerosol particles K. Zhang et al. 10.1080/02786826.2023.2245859
267. Versatile aerosol concentration enrichment system (VACES) operating as a cloud condensation nuclei (CCN) concentrator: development and laboratory characterization C. Dameto de España et al. 10.5194/amt-12-4733-2019
268. On the submicron aerosol distributions and CCN activity in and around the Korean Peninsula measured onboard the NASA DC-8 research aircraft during the KORUS-AQ field campaign M. Park et al. 10.1016/j.atmosres.2020.105004
269. Impact of monsoon on below cloud base aerosol hygroscopicity over a rain shadow region of India M. Varghese et al. 10.1016/j.atmosres.2023.106630
270. Impact of aerosol composition on cloud condensation nuclei activity Q. Zhang et al. 10.5194/acp-12-3783-2012
271. Hygroscopicity and composition of Alaskan Arctic CCN during April 2008 R. Moore et al. 10.5194/acp-11-11807-2011
272. CCN Properties of Organic Aerosol Collected Below and within Marine Stratocumulus Clouds near Monterey, California A. Asa-Awuku et al. 10.3390/atmos6111590
273. Influence of cloud processing on CCN activation behaviour in the Thuringian Forest, Germany during HCCT-2010 S. Henning et al. 10.5194/acp-14-7859-2014
274. The Dynamic Shape Factor of Sodium Chloride Nanoparticles as Regulated by Drying Rate Z. Wang et al. 10.1080/02786826.2010.503204
275. Influences of aerosol physiochemical properties and new particle formation on CCN activity from observation at a suburban site of China Y. Li et al. 10.1016/j.atmosres.2017.01.009
276. Cloud condensation nuclei characteristics during the Indian summer monsoon over a rain-shadow region V. Jayachandran et al. 10.5194/acp-20-7307-2020
277. The analysis of size-segregated cloud condensation nuclei counter (CCNC) data and its implications for cloud droplet activation M. Paramonov et al. 10.5194/acp-13-10285-2013
278. Hygroscopicity of nitrogen-containing organic carbon compounds: o-aminophenol and p-aminophenol K. Malek et al. 10.1039/D2EM00163B
279. Development and Application of a Wide Dynamic Range and High Resolution Atmospheric Aerosol Water-Based Supersaturation Condensation Growth Measurement System J. Bian et al. 10.3390/atmos12050558
280. The Amazon Tall Tower Observatory (ATTO): overview of pilot measurements on ecosystem ecology, meteorology, trace gases, and aerosols M. Andreae et al. 10.5194/acp-15-10723-2015
281. Water uptake by fresh Indonesian peat burning particles is limited by water-soluble organic matter J. Chen et al. 10.5194/acp-17-11591-2017
282. Significantly Enhanced Aerosol CCN Activity and Number Concentrations by Nucleation‐Initiated Haze Events: A Case Study in Urban Beijing F. Zhang et al. 10.1029/2019JD031457
283. Highly Biased Hygroscopicity Derived from Size-Resolved Cloud Condensation Nuclei Activation Ratios without Data Inversion D. Zhao-Ze & R. Liang 10.1080/16742834.2014.11447170
284. Hygroscopic growth of water soluble organic carbon isolated from atmospheric aerosol collected at US national parks and Storm Peak Laboratory N. Taylor et al. 10.5194/acp-17-2555-2017
285. Size-resolved observations of refractory black carbon particles in cloud droplets at a marine boundary layer site J. Schroder et al. 10.5194/acp-15-1367-2015
286. Water uptake of clay and desert dust aerosol particles at sub- and supersaturated water vapor conditions H. Herich et al. 10.1039/b901585j
287. Investigation on the hygroscopicity of oxalic acid and atmospherically relevant oxalate salts under sub- and supersaturated conditions S. Boreddy & K. Kawamura 10.1039/C8EM00053K
288. Aerosol characteristics and particle production in the upper troposphere over the Amazon Basin M. Andreae et al. 10.5194/acp-18-921-2018
289. Long-term observations of cloud condensation nuclei over the Amazon rain forest – Part 2: Variability and characteristics of biomass burning, long-range transport, and pristine rain forest aerosols M. Pöhlker et al. 10.5194/acp-18-10289-2018
290. Investigation of the effective peak supersaturation for liquid-phase clouds at the high-alpine site Jungfraujoch, Switzerland (3580 m a.s.l.) E. Hammer et al. 10.5194/acp-14-1123-2014
291. Impact of fatty acid coating on the CCN activity of sea salt particles Q. Nguyen et al. 10.1080/16000889.2017.1304064
292. Role of Aerosol Physicochemical Properties on Aerosol Hygroscopicity and Cloud Condensation Nuclei Activity in a Tropical Coastal Atmosphere A. T. C. et al. 10.1021/acsearthspacechem.2c00044
293. A synthesis of cloud condensation nuclei counter (CCNC) measurements within the EUCAARI network M. Paramonov et al. 10.5194/acp-15-12211-2015
294. Wildfire Smoke Particle Properties and Evolution, From Space-Based Multi-Angle Imaging II: The Williams Flats Fire during the FIREX-AQ Campaign K. Junghenn Noyes et al. 10.3390/rs12223823
295. Intercomparison of cloud condensation nuclei and hygroscopic fraction measurements: Coated soot particles investigated during the LACIS Experiment in November (LExNo) J. Snider et al. 10.1029/2009JD012618
296. Size-resolved and bulk activation properties of aerosols in the North China Plain Z. Deng et al. 10.5194/acp-11-3835-2011
297. Hygroscopic growth and droplet activation of soot particles: uncoated, succinic or sulfuric acid coated S. Henning et al. 10.5194/acp-12-4525-2012
298. Effects of aerosol organics on cloud condensation nucleus (CCN) concentration and first indirect aerosol effect J. Wang et al. 10.5194/acp-8-6325-2008
299. Measurements of aerosol and CCN properties in the Mackenzie River delta (Canadian Arctic) during spring–summer transition in May 2014 P. Herenz et al. 10.5194/acp-18-4477-2018
300. Aerosol hygroscopicity and cloud condensation nuclei activity during the AC<sup>3</sup>Exp campaign: implications for cloud condensation nuclei parameterization F. Zhang et al. 10.5194/acp-14-13423-2014
301. A new method for calculating number concentrations of cloud condensation nuclei based on measurements of a three-wavelength humidified nephelometer system J. Tao et al. 10.5194/amt-11-895-2018
302. Optical properties and cloud condensation nuclei activity of brown carbon containing α–dicarbonyls and reduced nitrogen compounds J. Zhou et al. 10.1016/j.atmosres.2023.106935
303. An improved parameterization scheme for size-resolved particle activation ratio and its application on comparison study of particle hygroscopicity measurements between HTDMA and DMA-CCNC J. Tao et al. 10.1016/j.atmosenv.2020.117403
304. New representation of water activity based on a single solute specific constant to parameterize the hygroscopic growth of aerosols in atmospheric models S. Metzger et al. 10.5194/acp-12-5429-2012
305. The challenge of simulating the sensitivity of the Amazonian cloud microstructure to cloud condensation nuclei number concentrations P. Polonik et al. 10.5194/acp-20-1591-2020
306. Use of lidar aerosol extinction and backscatter coefficients to estimate cloud condensation nuclei (CCN) concentrations in the southeast Atlantic E. Lenhardt et al. 10.5194/amt-16-2037-2023
307. Measurement report: Distinct size dependence and diurnal variation in organic aerosol hygroscopicity, volatility, and cloud condensation nuclei activity at a rural site in the Pearl River Delta (PRD) region, China M. Cai et al. 10.5194/acp-22-8117-2022
308. CCN activity and droplet growth kinetics of fresh and aged monoterpene secondary organic aerosol G. Engelhart et al. 10.5194/acp-8-3937-2008
309. Vertical profiles of cloud condensation nuclei number concentration and its empirical estimate from aerosol optical properties over the North China Plain R. Zhang et al. 10.5194/acp-22-14879-2022
310. Using Elemental Ratios to Predict the Density of Organic Material Composed of Carbon, Hydrogen, and Oxygen M. Kuwata et al. 10.1021/es202525q
311. Effect of Particle Morphology on Cloud Condensation Nuclei Activity M. Altaf et al. 10.1021/acsearthspacechem.7b00146
312. Rapid growth and high cloud-forming potential of anthropogenic sulfate aerosol in a thermal power plant plume during COVID lockdown in India A. Singh et al. 10.1038/s41612-023-00430-2
313. The evolution of cloud and aerosol microphysics at the summit of Mt. Tai, China J. Li et al. 10.5194/acp-20-13735-2020
314. Cloud condensation nuclei (CCN) activity analysis of low-hygroscopicity aerosols using the aerodynamic aerosol classifier (AAC) K. Gohil & A. Asa-Awuku 10.5194/amt-15-1007-2022
315. Characterization of aerosol hygroscopicity, mixing state, and CCN activity at a suburban site in the central North China Plain Y. Wang et al. 10.5194/acp-18-11739-2018
316. Altitude profiles of cloud condensation nuclei characteristics across the Indo-Gangetic Plain prior to the onset of the Indian summer monsoon V. Jayachandran et al. 10.5194/acp-20-561-2020
317. An examination of parameterizations for the CCN number concentration based on in situ measurements of aerosol activation properties in the North China Plain Z. Deng et al. 10.5194/acp-13-6227-2013
318. Nucleation-mode particle pool and large increases in <i>N</i><sub>cn</sub> and <i>N</i><sub>ccn</sub> observed over the northwestern Pacific Ocean in the spring of 2014 J. Wang et al. 10.5194/acp-19-8845-2019
319. Experimentally measured morphology of biomass burning aerosol and its impacts on CCN ability M. Giordano et al. 10.5194/acp-15-1807-2015
320. Direct Comparison of the Hygroscopic Properties of Ammonium Sulfate and Sodium Chloride Aerosol at Relative Humidities Approaching Saturation J. Walker et al. 10.1021/jp107802y
321. Seasonal variation of CCN concentrations and aerosol activation properties in boreal forest S. Sihto et al. 10.5194/acp-11-13269-2011
322. A modeling study of the aerosol effects on ice microphysics in convective cloud and precipitation development under different thermodynamic conditions H. Lee et al. 10.1016/j.atmosres.2014.03.022
323. Parameterization and comparative evaluation of the CCN number concentration on Mt. Huang, China S. Fang et al. 10.1016/j.atmosres.2016.07.004
324. Vertical profile of aerosol characteristics including activation over a rain shadow region in India M. Varghese et al. 10.1016/j.atmosenv.2021.118653
325. On the evaporation of ammonium sulfate solution W. Drisdell et al. 10.1073/pnas.0907988106
326. Cloud condensation nucleation activity of biomass burning aerosol M. Petters et al. 10.1029/2009JD012353
327. Effect of Sodium Dodecyl Benzene Sulfonate on the Production of Cloud Condensation Nuclei from Breaking Waves S. Hartery et al. 10.1021/acsearthspacechem.2c00230
328. Aerosol activation characteristics and prediction at the central European ACTRIS research station of Melpitz, Germany Y. Wang et al. 10.5194/acp-22-15943-2022
329. Recent developments in aerosol measurement techniques and the metrological issues S. Aggarwal 10.1007/s12647-010-0020-z
330. Rapid aerosol particle growth and increase of cloud condensation nucleus activity by secondary aerosol formation and condensation: A case study for regional air pollution in northeastern China A. Wiedensohler et al. 10.1029/2008JD010884
331. Hygroscopic properties of fresh and aged wood burning particles M. Martin et al. 10.1016/j.jaerosci.2012.08.006
332. Mixing state and compositional effects on CCN activity and droplet growth kinetics of size-resolved CCN in an urban environment L. Padró et al. 10.5194/acp-12-10239-2012
333. Role of droplet size classes on the cloud droplet spectral dispersion as observed over the Western Ghats K. Ansari et al. 10.1016/j.atmosres.2020.105104
334. Aerosol hygroscopicity and CCN activation kinetics in a boreal forest environment during the 2007 EUCAARI campaign K. Cerully et al. 10.5194/acp-11-12369-2011
335. Estimation of cloud condensation nuclei concentration from aerosol optical quantities: influential factors and uncertainties J. Liu & Z. Li 10.5194/acp-14-471-2014
336. Measurement report: Cloud processes and the transport of biological emissions affect southern ocean particle and cloud condensation nuclei concentrations K. Sanchez et al. 10.5194/acp-21-3427-2021
337. A new CCN activation parameterization and its potential influences on aerosol indirect effects Y. Wang et al. 10.1016/j.atmosres.2021.105491
338. Exploring CCN droplet suppression with a higher sensitivity optical particle counter E. Fofie et al. 10.1080/02786826.2017.1379592
339. Effects of surface tension time-evolution for CCN activation of a complex organic surfactant J. Lin et al. 10.1039/C9EM00426B
340. Optical Interrogation of Single Levitated Droplets in a Linear Quadrupole Trap by Cavity Ring-Down Spectroscopy A. Valenzuela et al. 10.1021/acs.jpca.0c09213
341. Airborne instruments to measure atmospheric aerosol particles, clouds and radiation: A cook's tour of mature and emerging technology D. Baumgardner et al. 10.1016/j.atmosres.2011.06.021
342. Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles Y. Li 10.1007/s00024-018-1903-0
343. Characterization of Aerosol Hygroscopicity Over the Northeast Pacific Ocean: Impacts on Prediction of CCN and Stratocumulus Cloud Droplet Number Concentrations B. Schulze et al. 10.1029/2020EA001098
344. First surface measurement of variation of Cloud Condensation Nuclei (CCN) concentration over the Pristine Himalayan region of Garhwal, Uttarakhand, India A. Gautam et al. 10.1016/j.atmosenv.2020.118123
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