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