scholarly journals Flux dynamics of planktic foraminiferal tests in the south-eastern Bay of Biscay (northeast Atlantic margin)

2013 ◽  
Vol 109-110 ◽  
pp. S169-S181 ◽  
Author(s):  
Tanja Kuhnt ◽  
Hélène Howa ◽  
Sabine Schmidt ◽  
Louis Marié ◽  
Ralf Schiebel
Ocean Science ◽  
2013 ◽  
Vol 9 (2) ◽  
pp. 399-410 ◽  
Author(s):  
A. Fontán ◽  
G. Esnaola ◽  
J. Sáenz ◽  
M. González

Abstract. Two high-frequency (HF) radar stations were installed on the coast of the south-eastern Bay of Biscay in 2009, providing high spatial and temporal resolution and large spatial coverage of currents in the area for the first time. This has made it possible to quantitatively assess the air–sea interaction patterns and timescales for the period 2009–2010. The analysis was conducted using the Barnett–Preisendorfer approach to canonical correlation analysis (CCA) of reanalysis surface winds and HF radar-derived surface currents. The CCA yields two canonical patterns: the first wind–current interaction pattern corresponds to the classical Ekman drift at the sea surface, whilst the second describes an anticyclonic/cyclonic surface circulation. The results obtained demonstrate that local winds play an important role in driving the upper water circulation. The wind–current interaction timescales are mainly related to diurnal breezes and synoptic variability. In particular, the breezes force diurnal currents in waters of the continental shelf and slope of the south-eastern Bay. It is concluded that the breezes may force diurnal currents over considerably wider areas than that covered by the HF radar, considering that the northern and southern continental shelves of the Bay exhibit stronger diurnal than annual wind amplitudes.


2013 ◽  
Vol 109-110 ◽  
pp. S105-S120 ◽  
Author(s):  
R. Somavilla ◽  
C. González-Pola ◽  
A. Lavín ◽  
C. Rodriguez

2009 ◽  
Vol 29 (8) ◽  
pp. 1123-1135 ◽  
Author(s):  
S. Retailleau ◽  
H. Howa ◽  
R. Schiebel ◽  
F. Lombard ◽  
F. Eynaud ◽  
...  

2007 ◽  
Vol 64 (6) ◽  
pp. 1136-1144 ◽  
Author(s):  
Deirdre Brophy ◽  
Pauline A. King

Abstract Brophy, D., and King, P. A. 2007. Larval otolith growth histories show evidence of stock structure in Northeast Atlantic blue whiting (Micromesistius poutassou). – ICES Journal of Marine Science, 64: 1136–1144. Oceanographic modelling studies suggest that blue whiting (Micromesistius poutassou) larvae released on the Northeast Atlantic spawning grounds split into two branches, one following a northerly drift trajectory and the second drifting towards the south. This mechanism is proposed to restrict gene flow between northern and southern stock components. This study examined larval growth histories recorded in otoliths of adult blue whiting from three regions of the main spawning area and three feeding areas for evidence of divergent dispersal pathways. Increment measurements show that fish from the south of the spawning area on average grew significantly faster as larvae than those from the north of the spawning area, confirming that blue whiting spawning west of Ireland and Scotland do not form a randomly mixing unit, and that larval dispersal influences the subsequent distribution of spawning adults. Larval otolith growth rates in feeding blue whiting from the Bay of Biscay were significantly faster than those of fish from the Norwegian Sea feeding grounds, showing that mixing of fish from these areas is limited. Fish from the Bay of Biscay grew faster as larvae than fish from all regions of the main spawning area. The results support the proposed split in the blue whiting stock and signal caution for managing the fishery.


2019 ◽  
Vol 180 ◽  
pp. 14-23 ◽  
Author(s):  
Igor Granado ◽  
Oihane C. Basurko ◽  
Anna Rubio ◽  
Luis Ferrer ◽  
Jerónimo Hernández-González ◽  
...  

2019 ◽  
Vol 12 (sup2) ◽  
pp. S111-S125 ◽  
Author(s):  
Amandine Declerck ◽  
M. Delpey ◽  
A. Rubio ◽  
L. Ferrer ◽  
O. C. Basurko ◽  
...  

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