Summary
The mean vertical ozone distribution as a function of season is computed from almost 6 years of regular soundings (three times per week) over Switzerland. By comparing the concurrent mean values of the total amount with the 35-year average at Arosa, and by using the correlation between ozone concentration at different levels with the total amount, adjusted values for the seasonal variation of the vertical ozone distribution are obtained which are thought to give a better representation of the long-term climatological mean. The data show a prominent biennial variation of the ozone content around the level of the maximum concentration which does not, however, show up in the total amount because it is missing in the lower stratosphere.
Similar content being viewed by others
References
H. U. Dütsch, W. Züllig andCh. Ch. Ling,Regular Ozone Observations as Thalwil, Switzerland, and Boulder, Colorado. Report LAPETH-1, Zürich 1970, 279 pp.
H. U. Dütsch, W. Züllig andCh. Ch. Ling, 1 1/2Years of routine observations of vertical ozone distribution near Zürich, Switzerland, Ann. Geophys.25 (1969), 249–260.
R. J. Reed,The present status of the 26-month oscillations, Bull. Am. Met. Soc.46 (1965), 376–387.
W. Züllig,Relation between the intensity of the stratospheric circumpolar vortex and the accumulation of ozone in the winter hemisphere, Pure and Appl. Geophys.106–108 (1973), 1544.
A. B. Pittock,Seasonal and year-to-year ozone variations from soundings over Southeastern Australia, Quart. J. Roy. Met. Soc.94 (1968), 563–575.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Dütsch, H.U., Ling, C.C. Six years of regular ozone soundings over Switzerland. PAGEOPH 106, 1151–1168 (1973). https://doi.org/10.1007/BF00881068
Published:
Issue Date:
DOI: https://doi.org/10.1007/BF00881068