. Fig. 145. The larval outburst in Weddell West and in the coastal waters of the East Wind drift as an annual event, a plotting based on data derived from annual observations covering the period November to March. Ice-edge February mean. (Fig. 147), one flowing parallel to and hugging the north-east coast, the other parallel to the south- west coast but much farther off the land. The extensive region between the south-west coast and the eastern boundary of the Weddell tongue flowing parallel to it is occupied by water (Deacon, ^933» P- iQij Fig- 11) principally of Bellingshausen Sea origin. Th
. Fig. 145. The larval outburst in Weddell West and in the coastal waters of the East Wind drift as an annual event, a plotting based on data derived from annual observations covering the period November to March. Ice-edge February mean. (Fig. 147), one flowing parallel to and hugging the north-east coast, the other parallel to the south- west coast but much farther off the land. The extensive region between the south-west coast and the eastern boundary of the Weddell tongue flowing parallel to it is occupied by water (Deacon, ^933» P- iQij Fig- 11) principally of Bellingshausen Sea origin. The current which carries the krill towards the island also carries the pack-ice, occasionally (p. 417, Fig. 148) as in September and October to within as little as 40 miles of its south-eastern tip.
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Keywords: ., bookcentury1900, booksubjectocean, booksubjectscientificexpediti
