A baroclinic western boundary current over a continental slope

Journal of Marine Research

Volumn 58, Issue 3, 2000, Pages 327-373

  Ford, R ^a  

^a IMPERIAL COLLEGE LONDON   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

BAROCLINIC MOTION; CIRCULATION MODELING; CONTINENTAL SLOPE; OCEANIC CIRCULATION; WESTERN BOUNDARY CURRENT;

EID: 0033826232     PISSN: 00222402     EISSN: None     Source Type: Journal    
DOI: 10.1357/002224000321511070     Document Type: Article

References (29)

1. On steady laminar flow with closed streamlines at large Reynolds numbers
2. On the mid-latitude circulation in a high-resolution model of the North Atlantic
3. On the utility and disutility of JEBAR
4. On the transport of the Gulf Stream between Cape Hatteras and the Grand Banks
5. Toward a parameterization of the eddy field near the Gulf Stream
6. The Northern Recirculation Gyre of the Gulf Stream
7. On the wind-driven circulation in an ocean with bottom topography
8. Baroclinic and topographic influences on the transport in western boundary currents
9. Gulf Stream structure, transport and recirculation near 68°W
10. The average distribution of volume transport and potential vorticity with temperature at three sections across the Gulf Stream
11. On the influence of the continental-slope on the western boundary-layer-the enhanced transport and recirculation
12. On the wind-driven ocean circulation
13. JEBAR, bottom pressure torque and Gulf Stream separation
14. Impact of wind forcing, bottom topography and inertia on midlatitude jet separation in a quasigeostrophic model
15. The oceanic thermocline and the associated thermohaline circulation
16. A two-layer Gulf Stream over a continental slope
17. Generalized two-layer models of ocean circulation
18. Large-scale semigeostrophic equations for use in ocean circulation models
19. A simple model of the joint effect of baroclinicity and relief
20. Joint effect of baroclinicity and bottom relief as an important factor in the dynamics of sea currents
21. On the North Atlantic circulation
22. Modelling ocean circulation with the large-scale semi-geostrophic equations
23. The westward intensification of wind-driven ocean currents
24. The effect of continental rises on the wind-driven ocean circulation
25. Wind-driven circulation in one- and two-layer oceans of variable depth