Measurements of eddy fluxes of momentum in the surface layer of the Gulf Stream
Further observations are reported, in which the action of eddies in the Florida Current produces a surface flux of momentum towards higher mean velocities. The results are thus in contrast to what would be expected if the eddies acted as a frictional dissipation mechanism. Furthermore, associated wi...
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| Veröffentlicht in: | Tellus 2012-01, Vol.17 (2), p.240-245 |
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| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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