Small fraction of marine cloud condensation nuclei made up of sea spray aerosol

• Published in: Nature geoscience Vol. 10; no. 9; pp. 674 - 679
• Main Authors: Quinn, P. K., Coffman, D. J., Johnson, J. E., Upchurch, L. M., Bates, T. S.
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 01-09-2017; Nature Publishing Group
• Subjects: 704/106/35/823; 704/106/35/824; 704/106/694/1108; Abundance; Aerosols; Boundary layers; Cloud condensation nuclei; Cloud properties; Clouds; Condensation; Condensation nuclei; Earth; Earth Sciences; Earth System Sciences; Entrainment; Geochemistry; Geology; Geophysics/Geodesy; Ice; Nuclei; Nucleus; Oceans; Properties; Radiation balance; Reflectance; Sea spray; Sea spray aerosols; Solar radiation; Spray; Sulfate aerosols; Sulfates; Supersaturation; Troposphere
• ISSN: 1752-0894; 1752-0908
• DOI: 10.1038/ngeo3003

Sea spray aerosols impact Earth’s radiation balance by directly scattering solar radiation. They also act as cloud condensation nuclei, thereby altering cloud properties including reflectivity, lifetime and extent. The influence of sea spray aerosol on cloud properties is thought to be particularly strong over remote ocean regions devoid of continental particles. Yet the contribution of sea spray aerosol to the population of cloud condensation nuclei in the marine boundary layer remains poorly understood. Here, using a lognormal-mode-fitting procedure, we isolate sea spray aerosols from measurements of particle size and abundance over the Pacific, Southern, Arctic and Atlantic oceans to determine the contribution of sea spray aerosol to the population of cloud condensation nuclei in the marine boundary layer. On a global basis, with the exception of the high southern latitudes, sea spray aerosol makes a contribution of less than 30% to the cloud condensation nuclei population for air that is supersaturated at 0.1 to 1.0%—the supersaturation range typical of marine boundary layer clouds. Instead, the cloud condensation nuclei population between 70° S and 80° N is composed primarily of non-sea-salt sulfate aerosols, due to large-scale meteorological features that result in entrainment of particles from the free troposphere.
Sea spray aerosols are thought to alter cloud properties in remote ocean regions. Aerosol analyses over four ocean regions reveal that these aerosols represent less than 30% of cloud condensation nuclei in typical marine boundary layer clouds.