Energy partition in the large-scale ocean circulation and the production of mid-ocean eddies

Deep-Sea Research and Oceanographic Abstracts

Volumn 21, Issue 7, 1974, Pages

  Gill, A E ^a   Green, J S A ^b   Simmons, A J ^c  

^a UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^b IMPERIAL COLLEGE LONDON   (United Kingdom)

^c UNIVERSITY OF READING   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

OCEANOGRAPHY;

EID: 0016082133     PISSN: 00117471     EISSN: None     Source Type: Journal    
DOI: 10.1016/0011-7471(74)90010-2     Document Type: Article

References (28)

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3. Large scale multi-buoy experiment in the Tropical Atlantic
4. Measurements of meridional heat transport by ocean currents
5. THE DYNAMICS OF LONG WAVES IN A BAROCLINIC WESTERLY CURRENT
6. On the Stability of Internal Baroclinic Jets in a Rotating Atmosphere
7. Velocity measurements in the deep water of the western North Atlantic: Summary
8. Long Waves and Cyclone Waves
9. A problem in baroclinic stability
10. Transfer properties of the large-scale eddies and the general circulation of the atmosphere
11. Note on the meridional transport of energy by the oceans
12. Meso-scale currents at a hydrophysical polygon in the tropical Atlantic
13. The Stability of Currents in the Atmosphere and the Ocean: Part I
14. Finite amplitude baroclinic waves
15. A SIMPLE THREE-DIMENSIONAL MODEL FOR THE STUDY OF LARGE-SCALE EXTRATROPICAL FLOW PATTERNS
16. Large-scale eddy motion in the western Atlantic
17. The baroclinic instability of a mid-ocean circulation
18. A time-sequence oceanographic investigation in the North Pacific trade-wind zone
19. The Aries Current Measurements in the Western North Atlantic
20. The Oscillations of the Atmosphere
21. New Estimate of Annual Poleward Energy Transport by Northern Hemisphere Oceans
22. Bermuda sea level in relation to tides, weather, and baroclinic fluctuations
23. The spectrum from two years to two minutes of temperature fluctuations in the main thermocline at Bermuda
24. The spectrum of ocean turbulence over distances between 40 and 1000 km