. Discovery reports. Discovery (Ship); Scientific expeditions; Ocean; Antarctica; Falkland Islands. 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 S^h IGI 14-11-27 s7°2i'eo"s , 46°43'3o"w + 2C 0- 100- 200- 300- 400- 500- G00 800 in £ ID00- H uJ z Id in z o <: 1500- o£ UJ 01 CO :20
. Discovery reports. Discovery (Ship); Scientific expeditions; Ocean; Antarctica; Falkland Islands. 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 S^h IGI 14-11-27 s7°2i'eo"s , 46°43'3o"w + 2C 0- 100- 200- 300- 400- 500- G00 800 in £ ID00- H uJ z Id in z o <: 1500- o£ UJ 01 CO :2000- 30OO-1. ST-* 151 16 - I - 27 53°25'00"S , 35° I5'00"W 1° 0° +1° +2°C 35 %c 335 -j â i i S : COLD ANTARCTIC SURFACE LAYER WARMER INTERMEDIATE WATER DEEP COLD 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 Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Institute of Oceanographic Sciences (Great Britain); National Institute of Oceanography of Great Britain; Great Britain. Colonial Office. Discovery Committee. London ; New York : Cambridge University Press
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