. Fig. 29. Surface density (a(): November 1929. little variation throughout the strait, the difference between the highest and lowest temperatures recorded amounting to only 0-53° C. The vertical sections from King George Island to Trinity Peninsula, Figs. 30-32, show a much greater development of the warm deep water at this end of the Bransfield Strait than in February. In February 1929 the only station on this line with a positive intermediate maximum temperature in this layer was St. WS 382, some 4 miles from King George Island, where a temperature of 0-53° C. was recorded at 400 m. The oth
. Fig. 29. Surface density (a(): November 1929. little variation throughout the strait, the difference between the highest and lowest temperatures recorded amounting to only 0-53° C. The vertical sections from King George Island to Trinity Peninsula, Figs. 30-32, show a much greater development of the warm deep water at this end of the Bransfield Strait than in February. In February 1929 the only station on this line with a positive intermediate maximum temperature in this layer was St. WS 382, some 4 miles from King George Island, where a temperature of 0-53° C. was recorded at 400 m. The other stations on the same line in February recorded only traces of intermediate thermal maxima and all of negative temperature. In November, however, on this line, positive 4-2
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