T. Vonclarmann et al., DETERMINATION OF THE STRATOSPHERIC ORGANIC CHLORINE BUDGET IN THE SPRING ARCTIC VORTEX FROM MIPAS-B LIMB EMISSION-SPECTRA AND AIR SAMPLING EXPERIMENTS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D7), 1995, pp. 13979-13997
Vertical profiles of halogenated source gases, CF2Cl2, CFCl3, CHF2Cl,
Cl-4, and CF4, were retrieved from limb emission spectra recorded by t
he Michelson Interferometer for Passive Atmospheric Sounding, Balloonb
orne version (MIPAS B) during a balloon flight launched from Esrange n
ear Kiruna, northern Sweden (68 degrees N) on March 14, 1992. This fli
ght was a contribution to the balloon launch program of the European A
rctic Stratospheric Ozone Experiment (EASOE) campaign. All problems en
countered during the analysis of the recorded spectra are discussed in
detail. These are primarily the lack of spectral data for HNO3 which
interferes with the CF2Cl2 nu(6) band, and the strong effects attribut
ed to the Pinatubo aerosol. As the air mass sounded by MIPAS was polar
vortex air, these data supplement the results of in situ air sampling
experiments, which investigated air masses outside or at the edge of
the polar vortex at altitudes below is km during the last phase of EAS
OE. An analysis is made of the vertical profiles of the seven most abu
ndant organic chlorine species (CF2Cl2, CFCl3, CHF2Cl, CCl4, CH3Cl, CH
3CCl3, and C2F3C3) during that phase of the EASOE campaign. Mixing rat
ios of those organic chlorine compounds which had not been measured by
MIPAS are inferred from profiles provided by air sampling experiments
performed between November 30, 1991, and March 12, 1992. These profil
es were adjusted to the dynamic conditions during the MIPAS observatio
ns, namely the effect of subsidence, using CF2Cl2 as a tracer. This al
lowed to derive the relative contributions of the organic chlorine spe
cies to the total chlorine budget of the air mass sounded by MIPAS. Th
e results are consistent with the high ClONO2 mixing ratio of 2.6 part
s per billion by volume (ppbv) observed at 18.9-km altitude during thi
s flight of MIPAS B.