Atlantic Water Circulation in the Canada Basin

ARCTIC ◽  
1974 ◽  
Vol 27 (4) ◽  
Author(s):  
J.L. Newton ◽  
L.K. Coachman
2020 ◽  
Vol 125 (8) ◽  
Author(s):  
Jianqiang Li ◽  
Robert S. Pickart ◽  
Peigen Lin ◽  
Frank Bahr ◽  
Kevin R. Arrigo ◽  
...  

Author(s):  
M. Karcher ◽  
F. Kauker ◽  
R. Gerdes ◽  
E. Hunke ◽  
J. Zhang

2018 ◽  
Vol 48 (2) ◽  
pp. 245-260 ◽  
Author(s):  
Hayley V. Dosser ◽  
Mary-Louise Timmermans

AbstractThe deep waters in the Canada Basin display a complex temperature and salinity structure, the evolution of which is poorly understood. The fundamental physical processes driving changes in these deep water masses are investigated using an inverse method based on tracer conservation combined with empirical orthogonal function analysis of repeat hydrographic measurements between 2003 and 2015. Changes in tracer fields in the deep Canada Basin are found to be dominated by along-isopycnal diffusion of water properties from the margins into the central basin, with advection by the large-scale Beaufort Gyre circulation as well as localized, vertical mixing playing important secondary roles. In the Barents Sea branch of the Atlantic Water layer, centered around 1200-m depth, diffusion is shown to be nearly twice as important as advection to lateral transport. Along-isopycnal diffusivity is estimated to be ~300–600 m2 s−1. Large-scale circulation patterns and lateral advective velocities associated with the anticyclonic Beaufort Gyre are inferred, with an average speed of 0.6 cm s−1. Below about 1500 m, along-isopycnal diffusivity is estimated to be ~200–400 m2 s−1.


2014 ◽  
Vol 44 (9) ◽  
pp. 2353-2369 ◽  
Author(s):  
Wenli Zhong ◽  
Jinping Zhao

Abstract In 2004, a cold mode of Atlantic Water (AW) entered the western Canada basin, replacing the anomalously warm AW that resided in the basin since the 1990s. This slightly colder AW was denser than the 1990s warm mode; it gradually filled most of the western basin by 2009. The enhanced surface stress curl led to the spinup of the Beaufort Gyre and convergence of freshwater. The spinup also resulted in a deepening of the AW core at the center of the gyre and in shoaling of the AW core at the margins of the gyre. The density versus depth relationship revealed in this study shows that the depth of the maximum AW temperature was mainly controlled by the density structure before 2007; thus, it is the case when the denser water was deeper and the case when the lighter water was shallower around the basin. However, this relationship was reversed to become the case when the denser water was shallower and the case when the lighter water was deeper since 2008 inside the Beaufort Gyre. The combined effect of density and sea ice retreat that enhanced surface stress curl determined the depth of the AW inside the Beaufort Gyre since 2008. The deepening of the AW core and expanding of the area where the AW deepening occurred had a profound effect on the large-scale circulation in the Arctic Ocean.


Author(s):  
Marylou Athanase ◽  
Christine Provost ◽  
Camila Artana ◽  
M. Dolores Pérez‐Hernández ◽  
Nathalie Sennéchael ◽  
...  

Author(s):  
Fiona A. McLaughlin ◽  
Eddy C. Carmack ◽  
William J. Williams ◽  
Sarah Zimmermann ◽  
Koji Shimada ◽  
...  

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