Transient adjustment of circulation in a midlatitude abyssal ocean basin with realistic geometry and bathymetry

Journal of Physical Oceanography

Volumn 31, Issue 3, 2001, Pages 725-745

  Curchitser, E N ^a   Haidvogel, D B ^a   Iskandarani, M ^a  

^a International Research Institute for Climate and Society   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BATHYMETRY; ENERGY DISSIPATION; TOPOLOGY;

TOPOGRAPHIC WAVES;

OCEANOGRAPHY;

ABYSSAL CIRCULATION; CIRCULATION MODELING; MIDLATITUDE ENVIRONMENT;

(EAST); MEDITERRANEAN SEA;

EID: 0035268320     PISSN: 00223670     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0485(2001)031<0725:TAOCIA>2.0.CO;2     Document Type: Article

References (16)

1. On the shallow water equations at low Reynolds number
2. On the transient adjustment of a mid-latitude abyssal ocean basin with realistic geometry: The constant depth limit
3. The energetically consistent shallow-water equations
4. Bouyancy-driven circulation in an ocean basin with isopycnals intersecting the sloping boundary
5. A staggered spectral finite element model for the shallow water equations
6. Boundary currents, free currents and dissipation in the low-frequency scattering of shelf waves
7. Establishment of deep ocean circulation driven by deep water production
8. Spinup of source-driven circulation in an abyssal basin n the presence of bottom topography
9. Eastern Mediterranean deep water renewal on the basis of chlorofluoromethane and tritium data
10. A tracer study of the thermohaline circulation of the Eastern Mediterranean
11. Recent changes in Eastern Mediterranean deep waters
12. On the abyssal circulation of the World Ocean 1: Stationary planetary flow patterns on a sphere
13. On the abyssal circulation of the world ocean II: An idealized model of the circulation pattern and amplitude in oceanic basins
14. Some examples of stationary planetary flow patterns in bounded basins
15. Effects of large-scale topography on abyssal circulation
16. Effects of planetary topography on the deep-sea circulation