Abstract
Ultraviolet (UV) lidar measurements of ozone have proven to possess a high level of reliabilty in the stratosphere. For measurements in the troposphere, however, a number of technical modifications is necessary. This is the conseguence of the lower ozone densities, which reguire the use of shorter, more strongly absorbed wavelengths than commonly applied in stratospheric systems, as well as of the enormous dynamical range of the backscattered light intensity.
© 1991 Optical Society of America
PDF ArticleMore Like This
H. Eisele and T. Trickl
TuC24 Optical Remote Sensing of the Atmosphere (ORS) 1995
Andrew O. Langford and Michael H. Proffitt
WC.3 Laser Applications to Chemical Analysis (LACSEA) 1994
N. SUGIMOTO, Y. SASANO, H. MAKANE, S. HAYASHIDA-AMANO, I. MATSUI, and A. MINATO
TUM2 Conference on Lasers and Electro-Optics (CLEO:S&I) 1989