Tropospheric BrO profiles (about 0.6+/-0.2 ppt, and 2.0+/-0.8 ppt at profil
e maximum) were measured for the first time. Our measurements add new infor
mation to recent speculations - based on indirect evidence - of BrO possibl
y being ubiquitous in the free troposphere [Harder. et al., 1998; Friess et
al., 1999; Van Roozendael et al., 1999; Pundt et al., 2000]. Our study rel
ies on a detailed comparison of BrO slant column densities (BrO-SCD) measur
ed in the troposphere from the LPMA/DOAS (Laboratoire de Physique Moleculai
re et Applications and Differential Optical Absorption Spectroscopy) gondol
a by direct Sun absorption, and BrO-SCD values subsequently measured in the
lowermost stratosphere during balloon ascent. The difference in total atmo
spheric BrO-SCDs measured in the troposphere and lowermost stratosphere - a
fter a suitable correction for the change in BrO due to photochemistry and
the observation geometry - is then attributed to tropospheric BrO.