§Vertical distribution
determines transport trajectories on the Bank: copepods in the surface waters (0- 15 m) are advected by Eckman transport.
§Copepods below the Eckman
layer are less subject to transport.
The tidal mixing front may help retain deeper-dwelling copepods on the Bank.
§Remaining deeper in the water
column may represent a strategy to aid retention and avoid loss from Georges Bank for small copepods like Pseudocalanus spp.