. ^T-- - -X- " --^T- Fig. 22. Graph showing the variation of the phosphate content from south to north at the depths of maximum temperature and salinity of the warm deep water in the Scotia Sea, north of the South Orkney Islands. Grande ridge, the warm deep water contains less phosphate than the intermediate current, and the maximum of the warm deep water is only 80-100 mg. compared with 120-140 mg. in the Antarctic intermediate current. In Plate V we have a good picture of the phosphate distribution along section 3 in the eastern part of the South Atlantic Ocean between 690 S and 30 N (S
. ^T-- - -X- " --^T- Fig. 22. Graph showing the variation of the phosphate content from south to north at the depths of maximum temperature and salinity of the warm deep water in the Scotia Sea, north of the South Orkney Islands. Grande ridge, the warm deep water contains less phosphate than the intermediate current, and the maximum of the warm deep water is only 80-100 mg. compared with 120-140 mg. in the Antarctic intermediate current. In Plate V we have a good picture of the phosphate distribution along section 3 in the eastern part of the South Atlantic Ocean between 690 S and 30 N (Sts. 1154-1184).
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Keywords: ., bookcentury1900, booksubjectocean, booksubjectscientificexpediti
