scholarly journals Spring Sea ice forecasts and Bering Sea Indigenous marine mammal harvests

2020 ◽  
Author(s):  
Olivia Lee ◽  
Lisa Sheffield Guy ◽  
Frank Johnson ◽  
Vera Metcalf ◽  
Hajo Eicken ◽  
...  
2016 ◽  
Vol 134 ◽  
pp. 157-172 ◽  
Author(s):  
Robert G. Campbell ◽  
Carin J. Ashjian ◽  
Evelyn B. Sherr ◽  
Barry F. Sherr ◽  
Michael W Lomas ◽  
...  

2020 ◽  
Vol 181-182 ◽  
pp. 104898 ◽  
Author(s):  
Bungo Nishizawa ◽  
Nodoka Yamada ◽  
Haruka Hayashi ◽  
Charlie Wright ◽  
Kathy Kuletz ◽  
...  

2016 ◽  
Vol 12 (9) ◽  
pp. 20160276 ◽  
Author(s):  
Martin Renner ◽  
Sigrid Salo ◽  
Lisa B. Eisner ◽  
Patrick H. Ressler ◽  
Carol Ladd ◽  
...  

Timing of spring sea-ice retreat shapes the southeast Bering Sea food web. We compared summer seabird densities and average bathymetry depth distributions between years with early (typically warm) and late (typically cold) ice retreat. Averaged over all seabird species, densities in early-ice-retreat-years were 10.1% (95% CI: 1.1–47.9%) of that in late-ice-retreat-years. In early-ice-retreat-years, surface-foraging species had increased numbers over the middle shelf (50–150 m) and reduced numbers over the shelf slope (200–500 m). Pursuit-diving seabirds showed a less clear trend. Euphausiids and the copepod Calanus marshallae/glacialis were 2.4 and 18.1 times less abundant in early-ice-retreat-years, respectively, whereas age-0 walleye pollock Gadus chalcogrammus near-surface densities were 51× higher in early-ice-retreat-years. Our results suggest a mechanistic understanding of how present and future changes in sea-ice-retreat timing may affect top predators like seabirds in the southeastern Bering Sea.


2012 ◽  
Vol 69 (7) ◽  
pp. 1180-1193 ◽  
Author(s):  
Zachary W. Brown ◽  
Kevin R. Arrigo

Abstract Brown, Z. W., and Arrigo, K. R. 2012. Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean. – ICES Journal of Marine Science, 69: . Satellite remote sensing data were used to examine recent trends in sea-ice cover and net primary productivity (NPP) in the Bering Sea and Arctic Ocean. In nearly all regions, diminished sea-ice cover significantly enhanced annual NPP, indicating that light-limitation predominates across the seasonally ice-covered waters of the northern hemisphere. However, long-term trends have not been uniform spatially. The seasonal ice pack of the Bering Sea has remained consistent over time, partially because of winter winds that have continued to carry frigid Arctic air southwards over the past six decades. Hence, apart from the “Arctic-like” Chirikov Basin (where sea-ice loss has driven a 30% increase in NPP), no secular trends are evident in Bering Sea NPP, which averaged 288 ± 26 Tg C year−1 over the satellite ocean colour record (1998–2009). Conversely, sea-ice cover in the Arctic Ocean has plummeted, extending the open-water growing season by 45 d in just 12 years, and promoting a 20% increase in NPP (range 441–585 Tg C year−1). Future sea-ice loss will likely stimulate additional NPP over the productive Bering Sea shelves, potentially reducing nutrient flux to the downstream western Arctic Ocean.


1985 ◽  
Vol 90 (C2) ◽  
pp. 3185 ◽  
Author(s):  
Robin D. Muench ◽  
James D. Schumacher

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