Sources of nitrate in stratocumulus cloud water: Airborne measurements during the 2011 E-PEACE and 2013 NiCE studies

Abstract

This study examines the sources of NO3− in stratocumulus clouds over the eastern Pacific Ocean off the California coast using airborne and surface measurement data from the Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE; 2011) and Nucleation in California Experiment (NiCE; 2013). Average NO3− air-equivalent concentrations in cloud water samples categorized as having been influenced by ship exhaust (2.5 μg m−3), strong marine emissions (2.5 μg m−3) and fires (2.0 μg m−3) were more than twice that in the background cloud water (0.9 μg m−3). During periods when biomass burning plumes resided above cloud top, 16 of 29 cloud water samples were impacted due to instability in the entrainment interface layer with NO3− levels reaching as high as 9.0 μg m−3. Nucleation scavenging of chloride depleted sea-salt is a source of cloud water NO3−, with the lowest Cl−:Na+ ratio (1.5) observed in ship-influenced samples. Surface aerosol measurements show that NO3− concentrations peak in the particle diameter range of 1.0–5.6 μm, similar to Na, Cl− and Si, suggesting that drop activation of crustal particles and sea salt could be an important source of NO3− in cloud water. The contrasting behavior of NO3− and SO42− is emphasized by the NO3−:SO42− mass concentration ratio which is highest in cloud water (by more than a factor of two) followed by above cloud aerosol, droplet residual particles, and below cloud aerosol. Trends of a decreasing NO3−:SO42− ratio with altitude in clouds are confirmed by parcel model studies due to the higher rate of in-cloud sulfate formation as compared to HNO3 uptake by droplets.