Archive image from page 49 of Discovery reports (1934) Discovery reports discoveryreports09inst Year: 1934 STATION SNOW Fig. 49. Vertical section of temperature: Snow Island to Trinity Island, December 1930. 549 550 551 552 500 IOOQi 1500- Fig. 50. Vertical section of density (ct(): Snow Island to Trinity Island, December 1930. WATER MOVEMENTS The treatment by dynamical methods of the data obtained from the various surveys of the Bransfield area has been a difficult task. As may be seen from the bathymetric chart, very great differences of depth occur at adjacent stations and it is imposs
Archive image from page 49 of Discovery reports (1934) Discovery reports discoveryreports09inst Year: 1934 STATION SNOW Fig. 49. Vertical section of temperature: Snow Island to Trinity Island, December 1930. 549 550 551 552 500 IOOQi 1500- Fig. 50. Vertical section of density (ct(): Snow Island to Trinity Island, December 1930. WATER MOVEMENTS The treatment by dynamical methods of the data obtained from the various surveys of the Bransfield area has been a difficult task. As may be seen from the bathymetric chart, very great differences of depth occur at adjacent stations and it is impossible from the present data to obtain sufficient figures from which satisfactory topographical charts may be drawn of the sea surface in relation (say) to the 2000 or 1500 decibar surfaces. Consequently some arbitrary treatment is necessary on account of the great differences
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