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Ollitrault, Michel; Gabillet, Céline; De Verdiere, Alain Colin. |
As two fluid particles separate in time, the entire spectrum of eddy motions is being sampled from the smallest to the largest scales. In large-scale geophysical systems for which the Earth rotation is important, it has been conjectured that the relative diffusivity should vary respectively as D-2 and D-4/3 for distances respectively smaller and larger than a well-defined forcing scale of the order of the internal Rossby radius (with D the r.m.s. separation distance). Particle paths data from a mid-latitude float experiment in the central part of the North Atlantic appear to support these statements partly: two particles initially separated by a few km within two distinct clusters west and east of the mid-Atlantic ridge, statistically dispersed following a... |
Tipo: Text |
Palavras-chave: Taylor dispersion; Dispersion; Atlantic circulation; Particule pairs. |
Ano: 2005 |
URL: http://archimer.ifremer.fr/doc/2005/publication-456.pdf |
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