Using the discharge flow-mass spectrometric technique, the kinetics and mechanism of the BrO + HO2 reaction have been investigated in the temperature range 233-344 K. With an excess of HO2 over BrO, the rate constant was found to be k(1) = (4.77 +/- 0.32) x 10(-12) exp[(580 +/- 100)/T] cm(3) molecule(-1) s(-1). The reaction may proceed via two channels : BrO + HO2 --> HOBr + O-2 (1a) and BrO + HO2 --> HBr + O-3 (1b). Over the whole temperature range, HOBr was observed as the major product, whereas an upper limit was measured for channel 1b from the absence of detection of O-3 : k(1b)/k(1) < 1.5%. The potential implications of these data are briefly discussed in relation to the stratospheric bromine/ozone interaction.