- Abstract:
-
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean overlying variable bottom topography. In the ocean interior we adopt a linear relation between potential vorticity, density and Montgomery potential, resulting in Welander's solution for an adiabatic internal thermocline. The horizontal structure of the circulation is described by a characteristic equation, obtained by imposing a boundary condition of no-normal flow at the sea floor and a presc...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1357/002224001321237344
-
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- Journal:
- JOURNAL OF MARINE RESEARCH
- Volume:
- 59
- Issue:
- 1
- Pages:
- 1-27
- Publication date:
- 2001-01-05
- DOI:
- EISSN:
-
1543-9542
- ISSN:
-
0022-2402
- URN:
-
uuid:876df6e0-9912-4a24-9400-dcbcea424474
- Source identifiers:
-
3488
- Local pid:
- pubs:3488
- Language:
- English
- Copyright date:
- 2001
Journal article
On the insensitivity of the wind-driven circulation to bottom topography
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