Reutter, P., Su, H., Trentmann, J., Simmel, M., Rose, D., Gunthe, S. S., . . . Pöschl, U. (2009). Aerosol- and updraft-limited regimes of cloud droplet formation: Influence of particle number, size and hygroscopicity on the activation of cloud condensation nuclei (CCN). Atmospheric Chemistry & Physics, 9(18), 7067. https://doi.org/10.5194/acp-9-7067-2009
Chicago Style (17th ed.) CitationReutter, P., H. Su, J. Trentmann, M. Simmel, D. Rose, S. S. Gunthe, H. Wernli, M. O. Andreae, and U. Pöschl. "Aerosol- and Updraft-limited Regimes of Cloud Droplet Formation: Influence of Particle Number, Size and Hygroscopicity on the Activation of Cloud Condensation Nuclei (CCN)." Atmospheric Chemistry & Physics 9, no. 18 (2009): 7067. https://doi.org/10.5194/acp-9-7067-2009.
MLA (9th ed.) CitationReutter, P., et al. "Aerosol- and Updraft-limited Regimes of Cloud Droplet Formation: Influence of Particle Number, Size and Hygroscopicity on the Activation of Cloud Condensation Nuclei (CCN)." Atmospheric Chemistry & Physics, vol. 9, no. 18, 2009, p. 7067, https://doi.org/10.5194/acp-9-7067-2009.