In 1995, concentrations of the chlorofluorocarbon compound CFC-12 in the ou
tflow water from the Persian Gulf were 8-40 fold higher than normally cause
d by air-sea gas exchange. At that time, the anomaly was restricted to the
Gulf of Oman north of 20 degrees N, while in 1998 the signal had spread sou
thwestward to 12 degrees N. The sources of this CFC-12 input of about 6400
kg are most likely the fire extinguishers and solvents used during and afte
r the Gulf War in 1991, This CFC-12 signal is a new feature of the Persian
Gulf Water (PGW) which can be used to track and quantify the spreading and
dilution of PGW in the northern Indian Ocean. The contaminated PGW spreads
southward with a mean velocity of 0.02-0.025 m s(-1). At 20 degrees N, the
anomaly is diluted by a factor of more than two, and east of the island Soc
otra by a factor of four. A mean transport of less than 0.5.10(6) m(3) s(-1
) is calculated for PGW assuming a mean dilution rate of 30% from the sourc
e signal in the Gulf of Oman to the western Arabian Sea.