Randomly-forced fluid flow in the presence of scale-unselective dissipation develops mean currents following topographic contours. Known mechanisms based on the scale-selective action of damping processes are not at work in this situation. Coarse-graining reveals that the phenomenon is a kind of noi
β¦ LIBER β¦
Dispersion and Mixing in Quasigeostrophic Turbulence
β Scribed by Bracco, Annalisa; von Hardenberg, Jost; Provenzale, Antonello; Weiss, Jeffrey B.; McWilliams, Jim C.
- Book ID
- 121735856
- Publisher
- The American Physical Society
- Year
- 2004
- Tongue
- English
- Weight
- 224 KB
- Volume
- 92
- Category
- Article
- ISSN
- 0031-9007
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