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ACP | Articles | Volume 18, issue 3
Atmos. Chem. Phys., 18, 1495–1506, 2018
https://doi.org/10.5194/acp-18-1495-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 18, 1495–1506, 2018
https://doi.org/10.5194/acp-18-1495-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 02 Feb 2018

Research article | 02 Feb 2018

Aerosol characteristics in the entrainment interface layer in relation to the marine boundary layer and free troposphere

Hossein Dadashazar et al.

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Cited articles

Alam, A., Shi, J. P., and Harrison, R. M.: Observations of new particle formation in urban air, J. Geophys. Res.-Atmos., 108, 4093, https://doi.org/10.1029/2001jd001417, 2003. 
Braun, R. A., Dadashazar, H., MacDonald, A. B., Aldhaif, A. M., Maudlin, L. C., Crosbie, E., Aghdam, M. A., Mardi, A. H., and Sorooshian, A.: Impact of wildfire emissions on chloride and bromide depletion in marine aerosol particles, Environ. Sci. Technol., 51, 9013–9021, 2017. 
Cai, R., Yang, D., Fu, Y., Wang, X., Li, X., Ma, Y., Hao, J., Zheng, J., and Jiang, J.: Aerosol surface area concentration: a governing factor for new particle formation in Beijing, Atmos. Chem. Phys., 17, 12327–12340, https://doi.org/10.5194/acp-17-12327-2017, 2017. 
Carman, J. K., Rossiter, D. L., Khelif, D., Jonsson, H. H., Faloona, I. C., and Chuang, P. Y.: Observational constraints on entrainment and the entrainment interface layer in stratocumulus, Atmos. Chem. Phys., 12, 11135–11152, https://doi.org/10.5194/acp-12-11135-2012, 2012. 
Caughey, S. J., Crease, B. A., and Roach, W. T.: A field-study of nocturnal stratocumulus, 2. Turbulence structure and entrainment, Q. J. Roy. Meteor. Soc., 108, 125–144, https://doi.org/10.1002/qj.49710845508, 1982. 
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This study shows with airborne data that in the thin layer above stratocumulus clouds, the entrainment interface layer (EIL), aerosol size distributions are influenced both by new particle formation and by pollutants above and below the EIL. These results are important with regard to understanding aerosol–cloud–climate interactions as the aerosol in this layer can influence the characteristics of stratocumulus clouds, which are the dominant cloud type by global area.
This study shows with airborne data that in the thin layer above stratocumulus clouds, the...
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