A53A-0353
Measurements of Atmospheric Aerosol Vertical Distributions above Svalbard, Norway using Unmanned Aerial Systems (UAS)
Friday, 18 December 2015
Poster Hall (Moscone South)
Timothy S Bates, University of Washington Seattle Campus, Seattle, WA, United States, James E Johnson, NOAA PMEL, Seattle, WA, United States, Scott Stalin, Pacific Marine Environmental Laboratory, Seattle, WA, United States, Hagen Telg, NOAA Boulder, Boulder, CO, United States, Daniel M Murphy, NOAA, Boulder, CO, United States, John F Burkhart, University of Oslo, Geosciences, Oslo, Norway; University of California, Merced, Sierra Nevada Research Institute, Merced, CA, United States, Patricia Quinn, NOAA Pacific Marine Environmental Laboratory, Seattle, WA, United States and Rune Storvold, Norut North Research Institute, Tromsø, Norway
Abstract:
Atmospheric aerosol vertical distributions were measured above Svalbard, Norway in April 2015 to investigate the processes controlling aerosol concentrations and radiative effects. The aerosol payload was flown in a NOAA/PMEL MANTA Unmanned Aerial System (UAS) on 9 flights totaling 19 flight hours. Measurements were made of particle number concentration and aerosol light absorption at three wavelengths, similar to those conducted in April 2011 (Bates et al., Atmos. Meas. Tech., 6, 2115-2120, 2013). A filter sample was collected on each flight for analyses of trace elements. Additional measurements in the aerosol payload in 2015 included aerosol size distributions obtained using a Printed Optical Particle Spectrometer (POPS) and aerosol optical depth obtained using a four wavelength miniature Scanning Aerosol Sun Photometer (miniSASP). The data show most of the column aerosol mass and resulting optical depth in the boundary layer but frequent aerosol layers aloft with high particle number concentration (2000 cm-3) and enhanced aerosol light absorption (1 Mm-1). Transport of these aerosol layers was assessed using FLEXPART particle dispersion models. The data contribute to an assessment of sources of BC to the Arctic and potential climate impacts.
