Particle chemical
composition affects aerosol optical
and physical
properties in ways important for the fate, transport, and impact of
atmospheric particulate matter. For example, hygroscopic constituents
take up water to increase the physical size of a particle, which can
alter the extinction properties and atmospheric lifetime. At the collocated
AERosol RObotic NETwork (AERONET) and Interagency Monitoring of PROtected
Visual Environments (IMPROVE) network monitoring stations in rural
Bondville, Illinois, we employ a novel cloudiness determination method
to compare measured aerosol physicochemical properties on predominantly
cloudy and clear sky days from 2010 to 2019. On cloudy days, aerosol
optical depth (AOD) is significantly higher than on clear sky days
in all seasons. Measured Ångström exponents are significantly
smaller on cloudy days, indicating physically larger average particle
size for the sampled populations in all seasons except winter. Mass
concentrations of fine particulate matter that include estimates of
aerosol liquid water (ALW) are higher on cloudy days in all seasons
but winter. More ALW on cloudy days is consistent with larger particle
sizes inferred from Ångström exponent measurements. Aerosol
chemical composition that affects hygroscopicity plays a determining
impact on cloudy versus clear sky differences in AOD, Ångström
exponents, and ALW. This work highlights the need for simultaneous
collocated, high-time-resolution measurements of both aerosol chemical
and physical properties, in particular at cloudy times when quantitative
understanding of tropospheric composition is most uncertain.