Removal of trace gases can both increase and decrease cloud droplet formation

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Authors: Elavarasi Ravichandran, Sanghee Han, Abigail S. Williams, Veronica Z. Berta, Jeremy L. Dedrick, Christian N. Pelayo, Nattamon Maneenoi, Lynn Monica Russell, Michael Wheeler, Jeremy J. B. Wentzell, John Liggio, Markus Dirk Petters
Cited by: 1
References: 100

Abstract

Aerosols consist of liquid or solid particles dispersed in a gas. Aerosol measurements generally rely on drying the particles before quantifying their physicochemical properties. This drying can potentially remove semivolatile compounds from the particles. Here, we show size-resolved cloud condensation nuclei (CCN) measurements quantifying the hygroscopicity parameter in the presence and absence of a denuder. The denuder efficiently removed alkanes and weakly functionalized acids, aldehydes, and alcohols with fewer than 10 carbon atoms from the gas phase. Denuding organic compounds perturbed the CCN-derived hygroscopicity parameter by up to 50%. Denuding either rendered the particles more or less CCN active, and the direction of the effect depended on sample relative humidity and trace gas concentration. The effect was weakest in early spring and strongest in late spring and summer. The measurements demonstrate an unexpectedly strong coupling between the particle and gas phase, influencing CCN activity through either volatilization or surface adsorption, or both.

Fields of Study & Subjects

Atmospheric chemistry and aerosols Atmospheric aerosols and clouds Particle Dynamics in Fluid Flows

Publication details

Journal / source
Science Advances
Publisher
American Association for the Advancement of Science (AAAS)
Volume
12
Issue
3
Pages
eadx0960–eadx0960
Publication date
14 January 2026
Language
EN