44 citations as recorded by crossref.

1. Opposite Aerosol Index-Cloud Droplet Effective Radius Correlations Over Major Industrial Regions and Their Adjacent Oceans X. Ma et al. 10.1029/2018GL077562
2. Influence of Common Assumptions Regarding Aerosol Composition and Mixing State on Predicted CCN Concentration M. Mahish et al. 10.3390/atmos9020054
3. 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
4. Improving our fundamental understanding of the role of aerosol−cloud interactions in the climate system J. Seinfeld et al. 10.1073/pnas.1514043113
5. Atmospheric new particle formation as a source of CCN in the eastern Mediterranean marine boundary layer N. Kalivitis et al. 10.5194/acp-15-9203-2015
6. Variation in global chemical composition of PM<sub>2.5</sub>: emerging results from SPARTAN G. Snider et al. 10.5194/acp-16-9629-2016
7. 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
8. SPARTAN: a global network to evaluate and enhance satellite-based estimates of ground-level particulate matter for global health applications G. Snider et al. 10.5194/amtd-7-7569-2014
9. Droplet activation properties of organic aerosols observed at an urban site during CalNex-LA F. Mei et al. 10.1002/jgrd.50285
10. Consistency and applicability of parameterization schemes for the size-resolved aerosol activation ratio based on field measurements in the North China Plain J. Tao et al. 10.1016/j.atmosenv.2017.11.021
11. Droplet number uncertainties associated with CCN: an assessment using observations and a global model adjoint R. Moore et al. 10.5194/acp-13-4235-2013
12. Air mass physiochemical characteristics over New Delhi: impacts on aerosol hygroscopicity and cloud condensation nuclei (CCN) formation Z. Arub et al. 10.5194/acp-20-6953-2020
13. 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
14. 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
15. Atmospheric new particle formation as source of CCN in the Eastern Mediterranean marine boundary layer N. Kalivitis et al. 10.5194/acpd-15-11143-2015
16. Droplet number prediction uncertainties from CCN: an integrated assessment using observations and a global adjoint model R. Moore et al. 10.5194/acpd-12-20483-2012
17. Study on CCN activity of fission product aerosols (CsI and CsOH) and their effect on size and other properties G. Mishra et al. 10.1016/j.atmosres.2019.104816
18. 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
19. 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/acpd-13-20419-2013
20. CCN closure study: Effects of aerosol chemical composition and mixing state D. Bhattu & S. Tripathi 10.1002/2014JD021978
21. Impact of mixing state and hygroscopicity on CCN activity of biomass burning aerosol in Amazonia M. Sánchez Gácita et al. 10.5194/acp-17-2373-2017
22. Uncertainty in Predicting CCN Activity of Aged and Primary Aerosols F. Zhang et al. 10.1002/2017JD027058
23. CCN Activity, Variability and Influence on Droplet Formation during the HygrA-Cd Campaign in Athens A. Bougiatioti et al. 10.3390/atmos8060108
24. CCN activity of organic aerosols observed downwind of urban emissions during CARES F. Mei et al. 10.5194/acpd-13-9355-2013
25. Worldwide data sets constrain the water vapor uptake coefficient in cloud formation T. Raatikainen et al. 10.1073/pnas.1219591110
26. CCN activity of organic aerosols observed downwind of urban emissions during CARES F. Mei et al. 10.5194/acp-13-12155-2013
27. External and internal cloud condensation nuclei (CCN) mixtures: controlled laboratory studies of varying mixing states D. Vu et al. 10.5194/amt-12-4277-2019
28. The Impact of Aerosol Particle Mixing State on the Hygroscopicity of Sea Spray Aerosol S. Schill et al. 10.1021/acscentsci.5b00174
29. 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
30. Size-resolved and integral measurements of cloud condensation nuclei (CCN) at the high-alpine site Jungfraujoch D. Rose et al. 10.5194/acpd-13-32575-2013
31. Inter-seasonal variability in size-resolved CCN properties at Kanpur, India D. Bhattu & S. Tripathi 10.1016/j.atmosenv.2013.12.016
32. Seasonal variability in chemical composition and source apportionment of sub-micron aerosol over a high altitude site in Western Ghats, India S. Mukherjee et al. 10.1016/j.atmosenv.2018.02.048
33. SPARTAN: a global network to evaluate and enhance satellite-based estimates of ground-level particulate matter for global health applications G. Snider et al. 10.5194/amt-8-505-2015
34. Assessment of cloud supersaturation by aerosol particle and cloud condensation nuclei (CCN) measurements M. Krüger et al. 10.5194/amtd-6-10021-2013
35. Measured and modelled Cloud Condensation Nuclei (CCN) concentration in São Paulo, Brazil: the importance of aerosol size-resolved chemical composition on CCN concentration prediction G. Almeida et al. 10.5194/acpd-13-32353-2013
36. Sources of primary and secondary organic aerosol and their diurnal variations M. Zheng et al. 10.1016/j.jhazmat.2013.10.047
37. Cloud condensation nuclei (CCN) and HR-ToF-AMS measurements at a coastal site in Hong Kong: size-resolved CCN activity and closure analysis J. Meng et al. 10.5194/acpd-14-9067-2014
38. Measured and modelled cloud condensation nuclei (CCN) concentration in São Paulo, Brazil: the importance of aerosol size-resolved chemical composition on CCN concentration prediction G. Almeida et al. 10.5194/acp-14-7559-2014
39. Phytoplankton blooms weakly influence the cloud forming ability of sea spray aerosol D. Collins et al. 10.1002/2016GL069922
40. A coupled observation – modeling approach for studying activation kinetics from measurements of CCN activity T. Raatikainen et al. 10.5194/acpd-12-1821-2012
41. A coupled observation – modeling approach for studying activation kinetics from measurements of CCN activity T. Raatikainen et al. 10.5194/acp-12-4227-2012
42. Spatial and seasonal variations of fine particle water-soluble organic carbon (WSOC) over the Southeastern United States: implications for secondary organic aerosol formation X. Zhang et al. 10.5194/acpd-12-9621-2012
43. Spatial and seasonal variations of fine particle water-soluble organic carbon (WSOC) over the southeastern United States: implications for secondary organic aerosol formation X. Zhang et al. 10.5194/acp-12-6593-2012
44. On the gas-particle partitioning of soluble organic aerosol in two urban atmospheres with contrasting emissions: 1. Bulk water-soluble organic carbon X. Zhang et al. 10.1029/2012JD017908