Articles | Volume 26, issue 20
https://doi.org/10.5194/acp-26-15201-2026
https://doi.org/10.5194/acp-26-15201-2026
Research article
 | 
29 Oct 2026
Research article |  | 29 Oct 2026

Spring-summer atmospheric circulation and boundary layer processes modulating aerosol and cloud characteristics over the coastal Northeast Pacific during EPCAPE

Seethala Chellappan, David Painemal, Mandana Thieman, Christian Pelayo, William L. Smith Jr., and Lynn M. Russell

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Cited articles

Abel, M. R. and Hall, A.: Local and synoptic mechanisms causing Southern California's Santa Ana winds, Clim. Dyn., 34, 847–857, https://doi.org/10.1007/s00382-009-0650-4, 2010. 
Beddows, D. C. S., Dall'osto, M., and Harrison, R. M.: An enhanced procedure for the merging of atmospheric particle size distribution data measured using electrical mobility and time-of-flight analysers, Aerosol Sci. Tech., 44, 11, https://doi.org/10.1080/02786826.2010.502159, 2010. 
Berta, V. Z., Han, S., Atsushi, O., Dedrick, J. L., Maneenoi, N., and Russell, L. M.: Aerosol quantification products at Mt. Soledad and Scripps Pier during EPCAPE 2023–24, in: Aerosol Microphysics and Chemical Measurements at Mt. Soledad and Scripps Pier during the Eastern Pacific Cloud Aerosol Precipitation Experiment (EPCAPE) from February 2023 to February 2024, UC San Diego Library Digital Collections [data set], https://doi.org/10.6075/J0WM1DSC, 2025. 
Bishop, C. M.: Neural Networks for Pattern Recognition, Oxford University Press, New York, ISBN 978-0-19-853849-3, 482 pp., 1995. 
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We analyzed observations from the ARM (Atmospheric Radiation Measurement) EPCAPE (Eastern Pacific Cloud Aerosol Precipitation Experiment) campaign at coastal California, and satellite cloud properties to understand how large-scale weather patterns influence marine low clouds and aerosols. Using ERA5 data and Self-Organizing Maps, we identified nine synoptic regimes linked to cloud cover, depth, and liquid water path. Satellite data show anticyclone position strongly affects cloud properties, while aerosol–cloud covariability depends on turbulence and supersaturation.
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