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Large-Eddy Simulations of Marine Boundary Layer Clouds Associated with Cold-Air Outbreaks during the ACTIVATE Campaign. Part II: Aerosol-Meteorology-Cloud Interaction
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Final Published Version
Author
Li, X.-Y.Wang, H.
Chen, J.
Endo, S.
Kirschler, S.
Voigt, C.
Crosbie, E.
Ziemba, L.D.
Painemal, D.
Cairns, B.
Hair, J.W.
Corral, A.F.
Robinson, C.
Dadashazar, H.
Sorooshian, A.
Chen, G.
Ferrare, R.A.
Kleb, M.M.
Liu, H.
Moore, R.
Scarino, A.J.
Shook, M.A.
Shingler, T.J.
Thornhill, K.L.
Tornow, F.
Xiao, H.
Zeng, X.
Affiliation
Department of Chemical and Environmental Engineering, The University of ArizonaDepartment of Hydrology and Atmospheric Sciences, The University of Arizona
Issue Date
2023-03-14
Metadata
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American Meteorological SocietyCitation
Li, X., and Coauthors, 2023: Large-Eddy Simulations of Marine Boundary Layer Clouds Associated with Cold-Air Outbreaks during the ACTIVATE Campaign. Part II: Aerosol–Meteorology–Cloud Interaction. J. Atmos. Sci., 80, 1025–1045, https://doi.org/10.1175/JAS-D-21-0324.1.Rights
© 2023 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Aerosol effects on micro/macrophysical properties of marine stratocumulus clouds over the western North Atlantic Ocean (WNAO) are investigated using in situ measurements and large-eddy simulations (LES) for two cold-air outbreak (CAO) cases (28 February and 1 March 2020) during the Aerosol Cloud Meteorology Interactions over the Western Atlantic Experiment (ACTIVATE). The LES is able to reproduce the vertical profiles of liquid water content (LWC), effective radius reff and cloud droplet number concentration Nc from fast cloud droplet probe (FCDP) in situ measurements for both cases. Furthermore, we show that aerosols affect cloud properties (Nc, reff, and LWC) via the prescribed bulk hygroscopicity of aerosols (k) and aerosol size distribution characteristics. Nc, reff, and liquid water path (LWP) are positively correlated to k and aerosol number concentration (Na) while cloud fractional cover (CFC) is insensitive to k and aerosol size distributions for the two cases. The realistic changes to aerosol size distribution (number concentration, width, and the geometrical diameter) with the same meteorology state allow us to investigate aerosol effects on cloud properties without meteorological feedback.We also use the LES results to evaluate cloud properties from two reanalysis products, ERA5 and MERRA-2. Compared to LES, the ERA5 is able to capture the time evolution of LWP and total cloud coverage within the study domain during both CAO cases whileMERRA-2 underestimates them. © 2023 American Meteorological Society.Note
6 month embargo; first published 14 March 2023ISSN
0022-4928Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1175/JAS-D-21-0324.1