HYDROLOGY 



north, for we meet Bellingshausen Sea water again in a strong stream, flowing in to- 

 wards the north of the island from the north-west. Part of this stream flows over the 

 continental shelf to the west forming an area of mixture with the Weddell Sea water, 

 which has come round from the south-east. After mixing with both Weddell Sea water 



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14-11-27 



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 COLD 



ANTARCTI C 



SURFACE LAYER 



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 ANTARCTIC WATER 



T 



Fig. 5. Temperature and salinity-depth curves at two stations within the Antarctic Zone, one to the south- 

 west and one to the north-east of South Georgia. 



