Mixing ratio profiles of ozone and several NO_y species were measured using the Limb Profile Monitor of the Atmosphere (LPMA) instrument during ascent, occultation and sunset for a balloon flight, which took place on August 21, 2001 from Kiruna (Sweden). These profiles were compared with the Reprobus 3D chemistry transport model (CTM) results for a latitude and a longitude area close to the mean balloon position. Discrepancies between model and measurements are observed particularly for the photochemical variation of NO_2 and NO between ascent and sunset. A more precise comparison, taking into account the variation with time of the position (latitude, longitude) of the probed air mass reduces the disagreement between model and measurements....