Abstract
Surface ozone data were obtained during September 1969 at an elevation of 3658 meters in the Colorado Rocky Mountains. These data indicate an early morning maximum and an early afternoon minimum of ozone. The data suggest that during the day air is brought to, the mountain top from below that is ozonedepleted. This would account for the distinct minimum of ozone in the afternoon. During the dark period the mountain criculation pattern is reversed and a maximum of ozone is seen.
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