Atmos. Meas. Tech., 9, 3893–3910, 2016 www.atmos-meas-tech.net/9/3893/2016/ doi:10.5194/amt-9-3893-2016 © Author(s) 2016. CC Attribution 3.0 License. The CU 2-D-MAX-DOAS instrument – Part 2: Raman scattering probability measurements and retrieval of aerosol optical properties Ivan Ortega1,2, Sean Coburn1,2, Larry K. Berg3, Kathy Lantz2,4, Joseph Michalsky2,4, Richard A. Ferrare5, Johnathan W. Hair5, Chris A. Hostetler5, and Rainer Volkamer1,2 1Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA 2Cooperative Institute for Research in Environmental Sciences (CIRES), Boulder, CO, USA 3Pacific Northwest National Laboratory, Richland, WA, USA 4Global Monitoring Division, Earth System Research Laboratory, NOAA, Boulder, CO, USA 5NASA Langley Research Center, Hampton, VA, USA Correspondence to: Rainer Volkamer (
[email protected]) Received: 8 December 2015 – Published in Atmos. Meas. Tech. Discuss.: 18 January 2016 Revised: 12 July 2016 – Accepted: 13 July 2016 – Published: 23 August 2016 Abstract. The multiannual global mean of aerosol optical retrievals of AOD430 and g with data from a co-located depth at 550 nm (AOD550/ over land is ∼ 0.19, and that over CIMEL sun photometer, Multi-Filter Rotating Shadowband oceans is ∼ 0.13. About 45 % of the Earth surface shows Radiometer (MFRSR), and an airborne High Spectral AOD550 smaller than 0.1. There is a need for measurement Resolution Lidar (HSRL-2). The average difference (rela- techniques that are optimized to measure aerosol optical tive to DOAS) for AOD430