F. Ferlemann et al., STRATOSPHERIC BRO PROFILES MEASURED AT DIFFERENT LATITUDES AND SEASONS - INSTRUMENT DESCRIPTION, SPECTRAL-ANALYSIS AND PROFILE RETRIEVAL, Geophysical research letters, 25(20), 1998, pp. 3847-3850
Measurements of stratospheric BrO profiles are reported using a novel
DOAS instrument (Differential Optical Absorption Spectrometry) operate
d on the LPMA/DOAS balloon gondola (LPMA/Laboratoire de Physique Molec
ulaire et Applications) during three flights (Leon, Nov. 23, 1998, Kir
una, Feb. 14, 1997, and Gap, June 20,1997). BrO was detected by its vi
brational bands (4-0 at 354.7 nm; 5-0 at 348.8 nm) of the A((2)pi)<--X
((2)pi) transition in direct sunlight spectra from balloon ascent, des
cent and during solar occultation at maximum (float) altitude. We show
that our accuracy is about +/-18% (1 sigma) during balloon ascent (so
lar zenith angles, SZA < 88 degrees), and about +/-25% for solar occul
tation measurements. For altitudes above the balloon float our observa
tions indicate average BrO mixing ratios of (14.4+/-2.5)ppt, (15.6+/-2
.8)ppt, and (15.3+/-2.8)ppt above 30.0 km, 30.0 km, and 39.8 km, respe
ctively.