Abstract:
The aerosol backscattering coefficient βπ in a surface atmospheric layer is calculated at the emission lines of NH3 and CO2 lasers (9 – 13.5 μm). It is shown that the coefficients βπ at the emission lines of an NH3 laser (11 – 13.5 μm) are comparable with the coefficients βπ at the emission lines of a CO2 laser near 10.6 μm. The dependence of βπ on the humidity and type of aerosols is studied. It is also shown that the coefficient βπ in a surface atmospheric layer at the lasing of an NH3 laser varies from 10-10 to 7×10-9 cm-1 sr-1. The lidar aerosol ratio is calculated as a function of the mean aerosol radius. It is found that this ratio is independent of the particle size for aerosol particles of radius exceeding 40 μm for the 11.7-μm aP(4,0) line of the ammonia laser.