Abstract
A review is presented of the results of laser-radar measurements made on the atmosphere at altitudes between 10 and 100 km. The theory of the method is discussed in relation to the scattering properties of the atmosphere. The variations in atmospheric temperature and density which are believed to occur are outlined and the limitations in the present knowledge discussed. A brief account is also given of the results of observations on atmospheric aerosols by methods other than the laser radar. The results from laser radar studies are examined and critically discussed in relation to atmospheric models. Emphasis is placed upon the evaluation of this method for providing the information about 1. (a) aerosol content, 2. (b) atmospheric density and its variations, and 3. (c) atmospheric composition.
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