1Laboratoire de l'Atmosphère et des Cyclones, Université de la Réunion, CNRS-INSU, UMR 8105, St.-Denis, Reunion Island, France
2Laboratoire Atmosphères, Milieux, Observations Spatiales, Université Versailles St.-Quentin, CNRS-INSU, Verrières-le-Buisson, France
Received: 02 Dec 2009 – Discussion started: 20 Jan 2010
Abstract. In this paper, the stellar occultation instrument GOMOS is compared with ozonesondes from the SHADOZ network. We only used nighttime O3 profiles and selected 8 Southern Hemisphere stations. 7 years of GOMOS datasets (GOPR 6.0cf and IPF 5.0) and 11 years of balloon-sondes are used in this study. A monthly distribution of GOMOS O3 mixing ratios was performed in the upper-troposphere and in the stratosphere (15–50 km). A comparison with SHADOZ was made in the altitude range between 15 km and 30 km.
Revised: 12 Jul 2010 – Accepted: 06 Aug 2010 – Published: 30 Aug 2010
In the 21–30 km altitude range, a satisfactory agreement was observed between GOMOS and SHADOZ, although some differences were observed depending on the station. The range for monthly differences generally decreases with increasing height and is within ±15%. It was found that the agreement between GOMOS and SHADOZ declines below ~20 km. The median differences are almost within ±5%, particularly above 23 km. But a large positive bias was found below 21 km, in comparison to SHADOZ.
Mze, N., Hauchecorne, A., Bencherif, H., Dalaudier, F., and Bertaux, J.-L.: Climatology and comparison of ozone from ENVISAT/GOMOS and SHADOZ/balloon-sonde observations in the southern tropics, Atmos. Chem. Phys., 10, 8025-8035, doi:10.5194/acp-10-8025-2010, 2010.