Influence of natural and anthropogenic aerosols on cloud base droplet size distributions in clouds over the South China Sea and West Pacific

Cumulus clouds are common over maritime regions. They are important regulators of the global radiative energy budget and global hydrologic cycle, as well as a key contributor to the uncertainty in anthropogenic climate change projections due to uncertainty in aerosol-cloud interactions. These interactions are regionally specific owing to their strong influences on aerosol sources and meteorology. Here, our analysis focuses on the statistical properties of marine boundary layer (MBL) aerosol chemistry and the relationships of MBL aerosol to cumulus cloud properties just above cloud base as sampled in 2019 during the NASA Cloud, Aerosol and Monsoon Processes Philippines Experiment (CAMP2Ex). The aerosol and clouds were sampled by instruments on the NASA P-3 aircraft over three distinct maritime regions around the Philippines: the West Pacific, the South China Sea, and the Sulu Sea. Our analysis shows three primary sources influenced the aerosol chemical composition: clean marine (ocean source), industrial (Southeast Asia, Manila, and cargo and tanker ship emissions), and biomass burning (Borneo and Indonesia). The clean marine aerosol chemical composition had low values of all sampled chemical signatures, specifically median values of 2.2ĝ€¯μgĝ€¯m-3 of organics (ORG), 2.3ĝ€¯μgĝ€¯m-3 of SO4, 0.3ĝ€¯μgĝ€¯m-3 of NO3, 1.4ĝ€¯μgĝ€¯m-3 of NH4, 0.04ĝ€¯μgĝ€¯m-3 of Cl, and 0.0074ĝ€¯μgĝ€¯m-3 of refractory black carbon (BC). Chemical signatures of the other two aerosol source regions were industrial, with elevated SO4 having a median value of 6.1ĝ€¯μgĝ€¯m-3, and biomass burning, with elevated median concentrations of ORG 21.2ĝ€¯μgĝ€¯m-3 and BC 0.1351ĝ€¯μgĝ€¯m-3. Based on chemical signatures, the industrial component was primarily from ship emissions, which were sampled within 60ĝ€¯km of ships and within projected ship plumes. Normalized cloud droplet size distributions in clouds sampled near the MBL passes of the P-3 showed that clouds impacted by industrial and biomass burning contained higher concentrations of cloud droplets, by as much as 1.5 orders of magnitude for diameters <ĝ€¯13ĝ€¯μm compared to clean marine clouds, while at size ranges between 13.0-34.5ĝ€¯μm the median concentrations of cloud droplets in all aerosol categories were nearly an order of magnitude less than the clean marine category. In the droplet size bins centered at diameters >ĝ€¯34.5ĝ€¯μm concentrations were equal to, or slightly exceeded, the concentrations of the clean marine clouds. These analyses show that anthropogenic aerosols generated from industrial and biomass burning sources significantly influenced cloud base microphysical structure in the Philippine region enhancing the small droplet concentration and reducing the concentration of mid-sized droplets.