Climate change in the southeastern Bering Sea: impacts on pollock stocks and implications for the oscillating control hypothesis
By K. Coyle, L. Eisner, F. Mueter, A. Pinchuk, M. Janout, K. Cieciel, E. Farley, Alexander G. Andrews. 2011
225 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/49837d68995dea7757addd84ce70ccfdf8766246
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Citations in the corpus
- Developing an acoustic survey of euphausiids to understand trophic interactions in the Bering Sea ecosystem (2012, background): “In contrast, very cold conditions have prevailed since 2006 (Stabeno et al., 2012), and increases in the abundance of both large copepods and euphausiids during that time have been documented (this study; Coyle et al., 2011; Hunt et al., 2011).”
- Krill, climate, and contrasting future scenarios for Arctic and Antarctic fisheries (2014, background): “A different pattern has been observed in the Bering Sea, where warmer than average temperatures have been associated with low krill abundance (Coyle et al., 2011; Hunt et al., 2011) and recent cold years with increases in krill abundance and the southward movement of boreal amphipod species…”
- Pelagic fish and zooplankton species assemblages in relation to water mass characteristics in the northern Bering and southeast Chukchi seas (2012, background): “In the SE Bering Sea, warm climate conditions were associated with smaller zooplankton in the water and in the prey base for juvenile salmon and age-0 pollock compared to cold climate conditions when larger lipid-rich zooplankton were more prevalent (Coyle et al. 2008, 2011).”
- Potential movement of fish and shellfish stocks from the sub-Arctic to the Arctic Ocean (2013, background): “In the southeastern Bering Sea, observations show that Calanus marshallae populations declined in warm temperatures and small less lipid-rich species of copepods increased (Coyle et al., 2011).”