During the EASOE (European Arctic Stratospheric Ozone Experiment) winter campaign 1991/92, first measurements were made from an aircraft with the new atmospheric sounder MIPAS‐FT (Michelson Interferometer for Passive Atmospheric Sounding ‐ Flugzeug Transall). The instrument measures infrared radiation emitted by atmospheric trace constituents in the spectral range between 750 and 1250 cm −1 . As first results, we present zenith column amounts of O 3 and HNO 3 retrieved from data recorded between January 30 and February 16, 1992 in the region from 45° west to 45° east and from 55° to 80° north. The column amounts vary considerably, from 1 to 3 × 10 16 molecules/cm² for HNO 3 and from 180 to 420 DU for O 3 , respectively. The strong linear correlation between these stratospheric gases indicates that the large variations during that period are mainly due to dynamic processes in the arctic atmosphere.
No takes yet. Share an insight, caveat, or question.
Blom et al. (1994) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: