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Modelling studies
suggest that the eastern GOM (strong
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influence of SS
and/or Slope water) a major source of
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near-surface
copepods to the NEP
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Western GOM
populations supply the crest of GB during
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winter
wind-driven flows
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These studies
used climatological winds - do not capture
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variability in
2-15 d band, or interannual variability
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