Abstract. Vertical profiles of the rate of linear change (trend) in the altitude range 15–50 km are determined from decadal O₃ time series obtained from SCIAMACHY¹/ENVISAT² measurements in limb-viewing geometry. The trends are calculated by using a multivariate linear regression. Seasonal variations, the quasi-biennial oscillation, signatures of the solar cycle and the El Niño–Southern Oscillation are accounted for in the regression. The time range of trend calculation is August 2002–April 2012. A focus for analysis are the zonal bands of 20° N–20° S (tropics), 60–50° N, and 50–60° S (midlatitudes). In the tropics, positive trends of up to 5% per decade between 20 and 30 km and negative trends of up to 10% per decade between 30 and 38 km are identified. Positive O₃ trends of around 5% per decade are found in the upper stratosphere in the tropics and at midlatitudes. Comparisons between SCIAMACHY and EOS MLS³ show reasonable agreement both in the tropics and at midlatitudes for most altitudes. In the tropics, measurements from OSIRIS⁴/Odin and SHADOZ⁵ are also analysed. These yield rates of linear change of O₃ similar to those from SCIAMACHY. However, the trends from SCIAMACHY near 34 km in the tropics are larger than MLS and OSIRIS by a factor of around two.



¹ SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY ² European environmental research satellite ³ Earth Observing System (EOS) Microwave Limb Sounder (MLS) ⁴ Optical Spectrograph and InfraRed Imager System ⁵ Southern Hemisphere ADditional OZonesondes