STRUCTURE OF THE SEDIMENTARY SECTION IN THE WESTERN BERING SEA

1987 ◽  
Vol 29 (12) ◽  
pp. 1438-1445 ◽  
Author(s):  
E. V. Shipilov
Keyword(s):  
Bering Sea ◽  
Western Bering Sea

Hydrography and biological resources in the western Bering Sea

2013 ◽  
Vol 94 ◽  
pp. 106-120 ◽  
Author(s):  
G.V. Khen ◽  
E.O. Basyuk ◽  
N.S. Vanin ◽  
V.I. Matveev
Keyword(s):  
Bering Sea ◽  
Biological Resources ◽  
Western Bering Sea

Water dynamics in the western Bering Sea and its impact on chlorophyll a concentration

2020 ◽  
Vol 70 (5) ◽  
pp. 593-602 ◽  
Author(s):  
Andrey G. Andreev ◽  
Maxim V. Budyansky ◽  
Gennady V. Khen ◽  
Michael Yu. Uleysky
Keyword(s):  
Chlorophyll A ◽  
Bering Sea ◽  
Water Dynamics ◽  
Chlorophyll A Concentration ◽  
Western Bering Sea

Ekman Transport and Zooplankton Concentration in the North Pacific Ocean

1967 ◽  
Vol 24 (3) ◽  
pp. 581-594 ◽  
Author(s):  
W. Percy Wickett
Keyword(s):  
Surface Water ◽  
Bering Sea ◽  
North Pacific ◽  
North Pacific Ocean ◽  
Ekman Transport ◽  
Sampling Area ◽  
The North ◽  
Western Bering Sea ◽  
North And South ◽  
The North Pacific

Annual concentrations of zooplankton off California varied directly, and concentrations in the western Bering Sea varied indirectly with calculated southerly components of Ekman transport in the previous year at 50°N,140°W. This point is in the area in which surface subarctic water and the deeper currents divide north and south. The underlying geostrophic flow requires approximately 1 year to reach each downstream sampling area. Summer concentrations of zooplankton at Ocean Station P, 50°N,145°W, varied with southerly and westerly components at 50°N,160°W during the previous winter. Fifty to sixty per cent of the variance of the annual concentration in zooplankton appears to be due to advection of surface water.

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