Raman lidar measurements of aerosol extinction and backscattering 1. Methods and comparisons
- Hughes STX, NASA Goddard Space Flight Center, Greenbelt, Maryland (United States); Adhesion promotion at a homopolymer--solid interface using random heteropolymers
- Department of Physics, University of Maryland Baltimore County, Baltimore, Maryland (United States)
- NASA Goddard Space Flight Center, Greenbelt, Maryland (United States)
- Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, Maryland (United States)
This paper examines the aerosol backscattering and extinction profiles measured at night by the NASA Goddard Space Flight Center Scanning Raman Lidar (SRL) during the remote cloud sensing (RCS) intensive operations period (IOP) at the Department of Energy Atmospheric Radiation Measurement (ARM) southern Great Plains (SGP) site in April 1994. These lidar data are used to derive aerosol profiles for altitudes between 0.015 and 5 km. Since this lidar detects Raman scattering from nitrogen and oxygen molecules as well as the elastic scattering from molecules and aerosols, it measures both aerosol backscattering and extinction simultaneously. The aerosol extinction/backscattering ratio varied between approximately 30 sr and 75 sr at 351 nm. Aerosol optical thicknesses derived by integrating the lidar profiles of aerosol extinction measured at night between 0.1 and 5 km are found to be about 10{endash}40{percent} lower than those measured by a Sun photometer during the day. This difference is attributed to the contribution by stratospheric aerosols not included in the lidar estimates as well as to diurnal differences in aerosol properties and concentrations. Aerosol profiles close to the surface were acquired by pointing the lidar nearly horizontally. Measurements of aerosol scattering from a tower-mounted nephelometer are found to be 40{percent} lower than lidar measurements of aerosol extinction over a wide range of relative humidities even after accounting for the difference in wavelengths. The reasons for this difference are not clear but may be due to the inability of the nephelometer to accurately measure scattering by large particles. {copyright} 1998 American Geophysical Union
- OSTI ID:
- 298623
- Journal Information:
- Journal of Geophysical Research, Vol. 103, Issue D16; Other Information: PBD: Aug 1998
- Country of Publication:
- United States
- Language:
- English
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