Abstract
The possibility of a long term evolution for tropospheric ozone, connected to a rise of anthropogenic releases, raises the question of a human climatic action. In order to bring an experimental confirmation to photochemical theories, continuous CO and O 3 measurements were started in November at the Pic du Midi observatory (3000 m altitude in the Pyrenean range). The results obtained confirm the photochemical hypothesis about the ozone origin. An ozone maximum is found in summer, corresponding to a CO minimum, which agrees with the increase of the u.v. flux. The seasonal variation does not exceed 19% of the value integrated over the year, which limits to 20% the maximal stratospheric contribution. The standard diurnal variations show the existence of a variable lag (0–4 h) between the O 3 minimum and the CO maximum, which is interpreted as showing a photochemical O 3 formation in the afternoon in the air coming from the lower layers.
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