. Discovery reports. Discovery (Ship); Scientific expeditions; Ocean; Antarctica; Falkland Islands. 500 STATION SMITH Fig. 25. Vertical section of temperature: Brabant Island to Smith Island, February 1929 W539B W5397 W5396 WS395 2690 2680 2700 BRABANT 500m Fig. 26. Vertical section of density (ct(): Brabant Island to Smith Island, February 1929. other parts of the strait. It has originated in the west and consists of part of the Antarctic surface water which flows out of the Bellingshausen Sea. The greater part of this stream passes north of the South Shetland Islands and flows north-east
. Discovery reports. Discovery (Ship); Scientific expeditions; Ocean; Antarctica; Falkland Islands. 500 STATION SMITH Fig. 25. Vertical section of temperature: Brabant Island to Smith Island, February 1929 W539B W5397 W5396 WS395 2690 2680 2700 BRABANT 500m Fig. 26. Vertical section of density (ct(): Brabant Island to Smith Island, February 1929. other parts of the strait. It has originated in the west and consists of part of the Antarctic surface water which flows out of the Bellingshausen Sea. The greater part of this stream passes north of the South Shetland Islands and flows north-east through the Drake Passage. Some, however, enters the Bransfield Strait between Low and. 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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