Baroclinic Geostrophic Turbulence and Jets in the Laboratory
Baroclinic, geostrophic turbulence is random, chaotic flow characterized by significant vertical gradients in density (Bu << 1) in which rotation plays a major role (Ro << 1). In the presence of a large-scale background gradient of potential vorticity (a β-effect ), a symmetry-breaking o...
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| Format: | Others |
| Language: | English English |
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Florida State University
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| Online Access: | http://purl.flvc.org/fsu/fd/2018_Sp_Smith_fsu_0071E_14453_comp |