Spreading of Red Sea overflow waters in the Indian Ocean

Abstract. As a result of its remarkably high salinity and despite its small volume input, remnants of Red Sea Water (RSW) have been identified in the Agulhas Current, over 6000 km distant of their source. This provided the •notivation to investigate the long-terln mean spreading of RSW throughout he Indian Ocean, using a comprehensive s t of observations, taken from the National Oceanographic Data Center archives and from the World Ocean Circulation Experilnent Hydro-graphic Program for the Indian Ocean. After emerging from the Gulf of Aden into the Arabian Sea, RSW spreads predominantly southwestward along the Aft'lean continental slope, as indicated by strongly inclined isohalines across the Arabian Sea. There is some monsoo • variability, so that during the winter monsoon there is more RSW present in the Gulf of Aden and an intensification of southward spreading along the western boundary, between 12 ø and 5øN. Elsewhere the in-termedlate depth salinity field of the Indian Ocean appears relatively stationary. Between 5 ø and 10øS, in the region of the South Equatorial Current, isohalines of the RSW layer become quasi-zonal across the width of the Indian Ocean, only dipping southward toward the western boundary west of 50øE. South of here, there is a strong tongue of RSW spreading southward through the Mozambique Channel and into the Agulhas Current. These conclusions concur with previous localized investigations of intermediate water properties. Using a simple mixing model, the percentage of RSW throughout the Indian Ocean was quantified. It was found that the flux of salt into the Gulf of Aden fi'om the Red Sea is similar to that estimated to cross 32øS in the Agulhas Current. This result implies that all the RSW which is mixed into the interior of the Indian Ocean may eventually be exported at the western boundary. Furthermore, it implies that RSW is the dominant component of the salt budget for the intermediate layer and that input from the Indonesian Seas and via diapycnic processes are small. 1