Articles | Volume 22, issue 1
Atmos. Chem. Phys., 22, 335–354, 2022

Special issue: Marine aerosols, trace gases, and clouds over the North Atlantic...

Atmos. Chem. Phys., 22, 335–354, 2022
Research article
10 Jan 2022
Research article | 10 Jan 2022

Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic

Xiaojian Zheng et al.

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Cited articles

Albrecht, B. A., Bretherton, C. S., Johnson, D., Schubert, W. H., and Frisch, A. S.: The Atlantic Stratocumulus Transition Experiment - ASTEX, B. Am. Meteorol. Soc., 76, 889–904,<0889:TASTE>2.0.CO;2, 1995. 
ARM MET Handbook: ARM Surface Meteorology Systems (MET) Handbook, DOE ARM Climate Research Facility, U. S. Department of Energy, Office of Science, Office of Biological and Environmental Research, Atmospheric Radiation Measurement Facility, DOE/SC-ARM/TR-0861, 19 pp., available at: (last access: 21 August 2021), 2011. 
Atmospheric Radiation Measurement Data Center: Ground-based Measurements at ENA site​​​​​​​, ARM [data set], available at: (last access: 2 September 2021​​​​​​​), 2021a. 
Atmospheric Radiation Measurement Data Center: ECMWF model output at ENA site​​​​​​​, ARM [data set], available at: (last access: 2 September 2021), 2021b. 
Braun, R. A., Dadashazar, H., MacDonald, A. B., Crosbie, E., Jonsson, H. H., Woods, R. K., Flagan, R. C., Seinfeld, J. H., and Sorooshian, A.: Cloud Adiabaticity and Its Relationship to Marine Stratocumulus Characteristics Over the Northeast Pacific Ocean, J. Geophys. Res.-Atmos., 123, 13790–13806,, 2018. 
Short summary
This study uses ground-based observations to investigate the physical processes in the aerosol–cloud interactions in non-precipitating marine boundary layer clouds, over the eastern North Atlantic Ocean. Results show that the cloud responses to the aerosols are diminished with limited water vapor supply, while they are enhanced with increasing water vapor availability. The clouds are found to be most sensitive to the aerosols under sufficient water vapor and strong boundary layer turbulence.
Final-revised paper