Atmospheric and Oceanic Fluid Dynamics¶
Vallis, G. K. (2006). Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-Scale Circulation. Cambridge University Press.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Balanced Flow
- Gradient-wind balance retains trajectory curvature; quasi-geostrophic, nonlinear-balance, semigeostrophic, and potential-vorticity-inversion models preserve additional effects while maintaining diagnostic constraints.
This sourceAuthoritative unified treatment of rotating stratified flow, scaling, balance hierarchies, and atmosphere–ocean recurrence.
- Gradient-wind balance retains trajectory curvature; quasi-geostrophic, nonlinear-balance, semigeostrophic, and potential-vorticity-inversion models preserve additional effects while maintaining diagnostic constraints.
Verification¶
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Registry ID ref:52efcfd0e1d5 · see in the full table