. DECEMBER I 3 4 7 7 8 9 19 19 30 2119 2128 2137 2513 539 I640 2136 2139 537 W496 STATION ADOL 5 FURC 5 ⢠Fig. ii8. Developmental condition of the massed surface larvae and small whale food in the 11-20 mm. range in spring. For vertical scale see legend to Fig. 107. rates to be considered, an extremely slow one in the East Wind drift, a somewhat faster, although still rather slow, one in the north-going outflows from these high latitudes, and a rapid one in the more northerly latitudes affected by the Weddell stream. Farther east there are two further instances of East Wind influence in the W


. DECEMBER I 3 4 7 7 8 9 19 19 30 2119 2128 2137 2513 539 I640 2136 2139 537 W496 STATION ADOL 5 FURC 5 ⢠Fig. ii8. Developmental condition of the massed surface larvae and small whale food in the 11-20 mm. range in spring. For vertical scale see legend to Fig. 107. rates to be considered, an extremely slow one in the East Wind drift, a somewhat faster, although still rather slow, one in the north-going outflows from these high latitudes, and a rapid one in the more northerly latitudes affected by the Weddell stream. Farther east there are two further instances of East Wind influence in the West Wind zone, namely, north-east of the Ross Sea (November records) and west of Graham Land (October and November records). The eastern half of the Pacific sector, well covered by our observations, is barren or virtually barren of larval stages, but again all samples are outside the East Wind drift. The developmental condition of the principal concentrations of the massed surface larvae in spring is shown in Fig. 118 which, although based primarily on our pre-eminently abundant material I


Size: 4090px × 1222px
Photo credit: © The Bookworm Collection / Alamy / Afripics
License: Licensed
Model Released: No

Keywords: ., bookcentury1900, booksubjectocean, booksubjectscientificexpediti