Tritium distributions in Weddell Sea water masses

During the 1975 and 1976 International Weddell Sea Oceanographic Expeditions, samples were collected for analysis by the Mount Soledad Tritium Laboratory. Most samples were of near‐bottom water in the western and northern Weddell Sea. Some samples were also collected of Warm Deep Water, Winter Water, and surface water. Highest tritium concentrations in bottom water were found in the northern Weddell Sea and along the western continental shelf. This indicates that the most recently formed bottom water is in these areas. In the central Weddell Sea, concentrations were lower, indicating slower renewal of bottom water. An upper limit of 3.5 × 106 m3/s is obtained for the formation rate of Weddell Sea Bottom Water. This yields a production rate of about 7×106 m3/s for classical Antarctic Bottom Water. Surface water and Winter Water also showed a strong gradient in tritium concentrations between the central Weddell Sea and the continental shelf.