Bering Sea shelf seismic reflection records, 1967 (R/V Thompson)

1968 ◽  
Author(s):  
David William Scholl ◽  
David Moody Hopkins
Keyword(s):  
Bering Sea ◽  
Seismic Reflection ◽  
Bering Sea Shelf

Continuous seismic reflection profile records, SEA-9-78-BS cruise, northern Bering Sea

1979 ◽  
Author(s):  
Matthew C. Larsen ◽  
Hans Nelson ◽  
Devin R. Thor
Keyword(s):  
Bering Sea ◽  
Seismic Reflection ◽  
Seismic Reflection Profile ◽  
Northern Bering Sea ◽  
Reflection Profile

Continuous seismic reflection profile records, SEA 5-76-BS cruise, northern Bering Sea

1978 ◽  
Author(s):  
Hans Nelson ◽  
M.L. Holmes ◽  
D.R. Thor ◽  
J.L. Johnson
Keyword(s):  
Bering Sea ◽  
Seismic Reflection ◽  
Seismic Reflection Profile ◽  
Northern Bering Sea ◽  
Reflection Profile

Stratification on the Eastern Bering Sea shelf revisited

2012 ◽  
Vol 65-70 ◽  
pp. 72-83 ◽  
Author(s):  
Carol Ladd ◽  
Phyllis J. Stabeno
Keyword(s):  
Bering Sea ◽  
Eastern Bering Sea ◽  
Bering Sea Shelf

Structure and Evolution of Bering Sea Shelf South of St. Lawrence Island

AAPG Bulletin ◽  
1976 ◽  
Vol 60 ◽  
Author(s):  
Michael S. Marlow (2), David W. Sch
Keyword(s):  
Bering Sea ◽  
Bering Sea Shelf

scholarly journals Calanus on the Bering Sea shelf: probable cause for population declines during warm years

2017 ◽  
Vol 39 (2) ◽  
pp. 257-270 ◽  
Author(s):  
K. O. Coyle ◽  
G. A. Gibson
Keyword(s):  
Bering Sea ◽  
Population Declines ◽  
Bering Sea Shelf ◽  
The Bering Sea

scholarly journals Air-sea CO<sub>2</sub> fluxes on the Bering Sea shelf

2011 ◽  
Vol 8 (5) ◽  
pp. 1237-1253 ◽  
Author(s):  
N. R. Bates ◽  
J. T. Mathis ◽  
M. A. Jeffries
Keyword(s):  
Bering Sea ◽  
Atmospheric Co2 ◽  
Net Community Production ◽  
Phytoplankton Primary Production ◽  
Co2 Partial Pressure ◽  
Small Areas ◽  
Co2 Sink ◽  
Bering Sea Shelf ◽  
Seawater Pco2 ◽  
The Bering Sea

Abstract. There have been few previous studies of surface seawater CO2 partial pressure (pCO2) variability and air-sea CO2 gas exchange rates for the Bering Sea shelf. In 2008, spring and summertime observations were collected in the Bering Sea shelf as part of the Bering Sea Ecological Study (BEST). Our results indicate that the Bering Sea shelf was close to neutral in terms of CO2 sink-source status in springtime due to relatively small air-sea CO2 gradients (i.e., ΔpCO2 and sea-ice cover. However, by summertime, very low seawater pCO2 values were observed and much of the Bering Sea shelf became strongly undersaturated with respect to atmospheric CO2 concentrations. Thus the Bering Sea shelf transitions seasonally from mostly neutral conditions to a strong oceanic sink for atmospheric CO2 particularly in the "green belt" region of the Bering Sea where there are high rates of phytoplankton primary production (PP)and net community production (NCP). Ocean biological processes dominate the seasonal drawdown of seawater pCO2 for large areas of the Bering Sea shelf, with the effect partly countered by seasonal warming. In small areas of the Bering Sea shelf south of the Pribilof Islands and in the SE Bering Sea, seasonal warming is the dominant influence on seawater pCO2, shifting localized areas of the shelf from minor/neutral CO2 sink status to neutral/minor CO2 source status, in contrast to much of the Bering Sea shelf. Overall, we compute that the Bering Sea shelf CO2 sink in 2008 was 157 ± 35 Tg C yr−1 (Tg = 1012 g C) and thus a strong sink for CO2.

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