Antarctic Ocean and Resources Variability 1988
DOI: 10.1007/978-3-642-73724-4_21
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Formation of Antarctic Krill Concentrations in Relation to Hydrodynamic Processes and Social Behaviour

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Cited by 35 publications
(31 citation statements)
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“…BIOMASS, 1977;Everson & Goss, 1991;Murphy et al, 1997;Trathan et al, 1998). They are also often associated with oceanic fronts including the Southern Antarctic Circumpolar Current Front (SACCF) at South Georgia (Witek, Kalinowski & Grelowski, 1988;Miller & Hampton, 1989, Hofmann et al, 1998Trathan et al, 2003). Everson (1976Everson ( , 1977 suggested that enhanced primary productivity in regions of upwelling could be a key factor in krill distribution.…”
Section: (1) General Characteristicsmentioning
confidence: 99%
See 1 more Smart Citation
“…BIOMASS, 1977;Everson & Goss, 1991;Murphy et al, 1997;Trathan et al, 1998). They are also often associated with oceanic fronts including the Southern Antarctic Circumpolar Current Front (SACCF) at South Georgia (Witek, Kalinowski & Grelowski, 1988;Miller & Hampton, 1989, Hofmann et al, 1998Trathan et al, 2003). Everson (1976Everson ( , 1977 suggested that enhanced primary productivity in regions of upwelling could be a key factor in krill distribution.…”
Section: (1) General Characteristicsmentioning
confidence: 99%
“…By contrast, Witek, et al (1988) suggested that behavioural reactions to water velocity gradients tended to concentrate krill in quiescent areas to the side of strong flow fields (see also Macaulay, English & Mathisen, 1984) where plankton abundance is often high, possibly as a consequence of the stable water conditions. Atkinson et al (2004) have shown that krill abundance in the Southern Ocean is spatially correlated with summer phytoplankton concentrations at a coarse scale.…”
Section: (1) General Characteristicsmentioning
confidence: 99%
“…The thin line represents the 2000-m isobath. The areas of consistent Antarctic krill spawning, as identified in Marr (1962) Transport of krill from these regions to South Georgia is thought to be accomplished by largescale ocean currents (Priddle et al, 1988;Witek et al, 1988;Murphy et al, 2004b).…”
Section: Introductionmentioning
confidence: 99%
“…A coastal current flows towards the southwest, which may serve to advect zooplankton into or out of the study region . In the case of krill, previous studies have suggested that abundance may be enhanced in regions of high velocity gradients such as frontal zones, meanders, and eddies (Witek et al, 1988;Ichii et Modeling and empirical studies have suggested that offshelf circumpolar deep water is pumped up onto the shelf by the action of the Antarctic Circumpolar Current (ACC) primarily at points where the deep troughs bisecting the shelf meet the shelf break and where the shelf break is strongly curved (Dinniman and Klinck, 2004;Klinck et al, 2004); horizontal blue arrows indicate such locations. Larger blue arrow indicates the direction of flow of the ACC.…”
Section: Southern Ocean Global Ecosystems Dynamics (So Globec) Programentioning
confidence: 98%
“…Qualitative examinations of krill abundance in relation to dynamic topography have previously led to the suggestion that high krill abundance may be associated with regions of high velocity gradients and the sluggish currents associated with eddies and meanders (Witek et al, 1988;Brinton, 1991;Ichii et al, 1998), and that retention may contribute to the formation of regions of enhanced krill abundance. The main known retentive feature in the present study region is a large and persistent gyre situated over the northern shelf, where krill biomass was low in fall.…”
Section: 42c Environmental Associationsmentioning
confidence: 99%