Comparison of lidar and satellite measurements of vertical ozone distribution in the upper troposphere – stratosphere according to data for 2017

Ozone was sensed with lidar at wavelength pairs 299/341 and 308/353 nm, allowing the vertical ozone stratification to be monitored within the upper troposphere – lower stratosphere, and within the stratosphere. The ozone lidar sensing, performed according to the method of differential absorption and scattering, is compared with data of IASI/MetOp and AURA satellites, as well as with the midlatitude Krueger model.