Archive image from page 40 of Discovery reports (1934) Discovery reports discoveryreports09inst Year: 1934 HYDROLOGY OF THE BRANSFIELD STRAIT 29 completely mixed and homogeneous water of Weddell Sea origin was present. In the vertical temperature section the warm deep water is seen to extend across the strait as an attenuated wedge-shaped layer, the apex of the wedge sloping up towards Trinity Peninsula. STATION WS476 WS477 WS478 KING GEORGE I. WS479 2740 WS4B0 WS4BI WS482 2750 2760 3770 2775 TRINITY PENIN* '27 78 27791 500i ID0O 1500 2000 Fig. 32. Vertical section of density (<r(): Ki
Archive image from page 40 of Discovery reports (1934) Discovery reports discoveryreports09inst Year: 1934 HYDROLOGY OF THE BRANSFIELD STRAIT 29 completely mixed and homogeneous water of Weddell Sea origin was present. In the vertical temperature section the warm deep water is seen to extend across the strait as an attenuated wedge-shaped layer, the apex of the wedge sloping up towards Trinity Peninsula. STATION WS476 WS477 WS478 KING GEORGE I. WS479 2740 WS4B0 WS4BI WS482 2750 2760 3770 2775 TRINITY PENIN* '27 78 27791 500i ID0O 1500 2000 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
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