Slope control in Western boundary currents

Journal of Physical Oceanography

Volumn 31, Issue 11, 2001, Pages 3349-3360

  Lee, S K ^a   Pelegri J L ^a   Kroll, J ^a  

^a Samsung Heavy Industries   (South Korea)

Author keywords

[No Author keywords available]

Indexed keywords

OCEAN CURRENTS; STRESSES; TORQUE; VELOCITY;

GEOSTROPHIC FLOWS;

OCEANOGRAPHY;

BOTTOM TOPOGRAPHY; CONTINENTAL SLOPE; WESTERN BOUNDARY CURRENT;

EID: 0035510542     PISSN: 00223670     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0485(2001)031<3349:SCIWBC>2.0.CO;2     Document Type: Article

References (33)

1. The Gulf stream-barrier or blender
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3. Mean circulation in shallow seas
4. The arrested topographic wave
5. The pressure field along the Western margin of the North Atlantic
6. Ocean currents over the continental slope
7. Vorticity balance of boundary currents
8. The role of secondary circulation in boundary mixing
9. Boundary mixing and arrested Ekman layers: Rotating stratified flow near a sloping boundary
10. A laboratory study of the effects of a sloping side boundary on wind-driven calculation in a homogeneous ocean model
11. Linear theory of the effect of a sloping boundary on circulation in a homogeneous laboratory model
12. Baroclinic and topographic influences on the transport in Western boundary currents
13. The three-dimensional structure of wind-driven gyres: Ventilation and subduction
14. Slope currents and "JEBAR:
15. The bottom boundary layer over the Northern California shelf
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17. Slippery bottom boundary layers on a slope
18. On the wind-driven ocean circulation
19. A two-layer Gulf stream over a continental slope
20. Joint effect of baroclinicity and bottom relief as an important factor in the dynamics of ocean currents
21. Self-advection of density perturbations on a sloping continental shelf
22. On the joint effect of baroclinicity and topography
23. The westward intensification of wind-driven ocean currents
24. Current and temperature variability on the continental slope
25. The variability of mixing at the continental slope
26. Asymmetric behavior of an oceanic boundary layer above a sloping bottom
27. Topographic influences on the path of the Gulf stream
28. A study of the bottom boundary layer of the Florida current