1995
DOI: 10.1575/1912/5624
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Physical processes and zooplankton distribution in the Great South Channel : observational and numerical studies

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Cited by 4 publications
(3 citation statements)
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“…We discuss briefly examples of steady flows analogous to those used in previous treatments (e.g. [9,13]), before moving to time-dependent flows and to more realistic simulations relevant to the flows in the GOM.…”
Section: Concentration Of Depth-keeping Organisms By Fluid Flowmentioning
confidence: 99%
See 1 more Smart Citation
“…We discuss briefly examples of steady flows analogous to those used in previous treatments (e.g. [9,13]), before moving to time-dependent flows and to more realistic simulations relevant to the flows in the GOM.…”
Section: Concentration Of Depth-keeping Organisms By Fluid Flowmentioning
confidence: 99%
“…Previous papers have applied this idea, (e.g. [5,6,9,13,19]) but have focused more on analytical x-z flows whereas we are interested in flows with complex horizontal structure. As Appendix 1 shows, if the vertical swimming and its random variability overcome the fluid motions and cause clustering around the preferred depth, the biomass density can be represented asb(x, t)F(z) where…”
Section: Concentration Of Depth-keeping Organisms By Fluid Flowmentioning
confidence: 99%
“…Using net-tows, the densest patches were found to range in size from 100-1000 m across, while the vertical extent of these patches is in the range of 1-10 m , ). Observations of peak density within a patch are in the range of 103-104 copepods/m 3 , Beardsley et al (1996)), which is one to three orders-of-magnitude larger than typical values measured in the GOM in springtime (Epstein (1995), ). The temporal persistence of the patches is somewhere between hours and days, however what determines this time scale is unknown (M. Baumgartner, pers.…”
Section: Calanus Finmarchicus and The South Channel Ocean Productivitmentioning
confidence: 70%