Polarimeter + Lidar–Derived Aerosol Particle Number Concentration
Joseph S. Schlosser, Snorre Stamnes, S. P. Burton, Brian Cairns, Ewan Crosbie, Bastiaan van Diedenhoven, Glenn S. Diskin, Sanja Dmitrovic, R. A. Ferrare, Johnathan W. Hair, C. A. Hostetler, Yongxiang Hu, Xu Liu, Richard H. Moore, Taylor Shingler, Michael A. Shook, Kenneth L. Thornhill, Edward L. Winstead, Luke D. Ziemba, Armin Sorooshian
Abstract
In this study, we propose a simple method to derive vertically resolved aerosol particle number concentration ( N a ) using combined polarimetric and lidar remote sensing observations. This method relies on accurate polarimeter retrievals of the fine-mode column-averaged aerosol particle extinction cross section and accurate lidar measurements of vertically resolved aerosol particle extinction coefficient such as those provided by multiwavelength high spectral resolution lidar. We compare the resulting lidar + polarimeter vertically resolved N a product to in situ N a data collected by airborne instruments during the NASA aerosol cloud meteorology interactions over the western Atlantic experiment (ACTIVATE). Based on all 35 joint ACTIVATE flights in 2020, we find a total of 32 collocated in situ and remote sensing profiles that occur on 11 separate days, which contain a total of 322 cloud-free vertically resolved altitude bins of 150 m resolution. We demonstrate that the lidar + polarimeter N a agrees to within 106% for 90% of the 322 vertically resolved points. We also demonstrate similar agreement to within 121% for the polarimeter-derived column-averaged N a . We find that the range-normalized mean absolute deviation (NMAD) for the polarimeter-derived column-averaged N a is 21%, and the NMAD for the lidar + polarimeter-derived vertically resolved N a is 16%. Taken together, these findings suggest that the error in the polarimeter-only column-averaged N a and the lidar + polarimeter vertically resolved N a are of similar magnitude and represent a significant improvement upon current remote sensing estimates of N a .