2008
DOI: 10.1016/j.csr.2008.04.014
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Bowhead whales feed on plankton concentrated by estuarine and tidal currents in Academy Bay, Sea of Okhotsk

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Cited by 44 publications
(14 citation statements)
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“…The eddy had a radius of 8 km and was associated with elevated concentrations of zooplankton, represented mainly by C. glacialis and M. longa. The aggregation of C. glacialis due to anticyclonic eddy circulation has also been observed in Academy Bay in the Sea of Okhotsk (Rogachev et al 2008). Another eddy-like structure, with a cold-water core, was observed in the southern FZ sections.…”
Section: Discussionmentioning
confidence: 71%
“…The eddy had a radius of 8 km and was associated with elevated concentrations of zooplankton, represented mainly by C. glacialis and M. longa. The aggregation of C. glacialis due to anticyclonic eddy circulation has also been observed in Academy Bay in the Sea of Okhotsk (Rogachev et al 2008). Another eddy-like structure, with a cold-water core, was observed in the southern FZ sections.…”
Section: Discussionmentioning
confidence: 71%
“…A likely source of these prey is the Return Atlantic Current running in deeper waters just off the shelf (cf. Hirsche and Kwasniewski 1997), advecting copepods onto the shelf area of the NEW from the more productive eastern part of the Fram Strait (Hirsche et al 2006;Falk-Petersen et al 2015), a phenomenon observed in other shallow bowhead whale feeding areas (Rogachev et al 2008;Ashjian et al 2010;Walkusz et al 2012;Heide-Jørgensen et al 2013).…”
Section: Resultsmentioning
confidence: 98%
“…These productive sites attract a large grazing zooplankton biomass (Sakshaug 1997), among which are the lipid-rich copepods and euphausiids (Percy & Fife 1980, Falk-Petersen et al 1998) that are preyed on by bowhead whales (Marquette 1986, Lowry 1993. Bowhead whales have been observed feeding at the sea surface, within the water column, and benthically (Rogachev et al 2008). Prey density is unlikely the key feature controlling migration patterns since bowhead whales abandon highly productive areas in the Bering Sea and West Greenland during the peak spring plankton bloom to move into less productive Beaufort Sea and Arctic Archipelago, respectively (Lowry 1993).…”
Section: Discussionmentioning
confidence: 99%