Archive image from page 40 of Discovery reports (1934) Discovery reports discoveryreports09inst Year: 1934 Fig. 32. Vertical section of density (<r(): King George Island to Trinity Peninsula, November 1929. The vertical sections of the line between Livingston Island and Trinity Peninsula are shown in Figs. 33-5. As with the section farther to the north-east the densest surface STATION LIVINGSTON I. W5483 WS484 WS485 5C» ID00M 1500m WS486 WS487 3410. 34-20 TRINITY PENIN* Fig- 33- Vertical section of salinity: Livingston Island to Trinity Peninsula, November 1929. water is again found at
Archive image from page 40 of Discovery reports (1934) Discovery reports discoveryreports09inst Year: 1934 Fig. 32. Vertical section of density (<r(): King George Island to Trinity Peninsula, November 1929. The vertical sections of the line between Livingston Island and Trinity Peninsula are shown in Figs. 33-5. As with the section farther to the north-east the densest surface STATION LIVINGSTON I. W5483 WS484 WS485 5C» ID00M 1500m WS486 WS487 3410. 34-20 TRINITY PENIN* Fig- 33- Vertical section of salinity: Livingston Island to Trinity Peninsula, November 1929. water is again found at the station closest to Trinity Peninsula, St. WS 487. The com- plete vertical mixing which was found at the corresponding station, St. WS 480, on the King George Island line is not seen at St. WS 487. The warm deep water has its
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