Abstract

Tropospheric ozone measurements were performed at the Observatoire de Haute Provence (OHP) in Southern France by three instruments during the last 10 yr: Brewer Mast (BM) ozonesondes 1985/1991, ECC ozonesondes: 1991/1995, lidar: 1990/1995. The error analysis shows an overall accuracy of 10% for the BM sondes and lidar data, and 5% for the ECC sondes. A comparison of the tropospheric seasonal means above 3 km shows that the differences between the three instruments are within the instrument accuracy. The OHP ECC data are also compared to the 1976/1983 ozone measurements performed with BM sondes at the Biscarosse station also in Southern France to estimate possible tropospheric ozone changes during the 1980s. Yearly mean values imply a maximum annual ozone increasing rate of 8 ± 2% per decade in the 1980s, but this trend becomes insignificant if one includes the usual − 15% bias between BM and ECC. The shift of the seasonal variation from a spring maximum to a spring/summer maximum is however statistically significant during the 1980s. In the upper troposphere, the seasonal means are studied using a height scale relative to the tropopause, showing a similar seasonal variation than in the mid-troposphere. Also an increase of the ozone spring/summer maximum with the altitude is shown. A negative trend of − 10%/decade is inferred at the tropopause level using the OHP and Biscarosse data.

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