The stratospheric aerosol layer observed by lidar since October 1976. A contribution to the problem of hemispheric climate
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
http://link.springer.com/content/pdf/10.1007/BF02243739.pdf
Reference55 articles.
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3. Reiter, R., Sladkovic, R.: Control of Vertical Transport of Aerosols Between 700 and 3000 m by the Lapse Rate and Fine Structure of Temperature: Results of a Sequence of Measurements Covering Several Years. J. Geophys. Res.75, 3065 (1970).
4. Carnuth, W.: Aerosol Size Distribution at 700, 1800 and 3000 m a.s.l. J. Geophys. Res.75, 2999 (1970).
5. Reiter, R., Sladkovic, R., Pötzl, K., Carnuth, W., Kanter, H.-J.: Studies on the Influx of Stratospheric Air Into the Lower Troposphere Using Cosmic-Ray Produced Radionuclides and Fallout. Arch. Met. Geoph. Biokl., Ser. A20, 211–246 (1971).
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