Episodes of elevated bromine oxide (BrO) concentration are known to occur a
t high Latitudes in the Arctic boundary layer and to lead to catalytic dest
ruction of ozone at those latitudes; these events have not been observed at
Lower latitudes. With the use of differential optical absorption spectrosc
opy (DOAS), Locally high BrO concentrations were observed at mid-latitudes
at the Dead Sea, Israel, during spring 1997. Mixing ratios peaked daily at
around 80 parts per trillion around noon and were correlated with Low bound
ary-layer ozone mixing ratios.