VERTICAL DIFFUSION OF THE FAR WAKE OF A SPHERE MOVING IN A STRATIFIEDFLUID

The far wake of a sphere towed horizontally in a linearly stratified f luid with Froude numbers F is-an-element-of (0.25,12.7) and Reynolds n umbers Re is-an-element-of [150,30 000] is investigated. Regardless of the initial Froude number, the wake becomes quasi two dimensional at times large compared with the Brunt-Vaisala period. For F less-than-or -equal-to 4.5, the horizontal motions are coherent over the whole dept h of the wake. The wake takes the form of a regular von Karman street for F less-than-or-equal-to 1.5 but is irregular at larger F. For F gr eater-than-or-equal-to 4.5 the far wake consists of, vertically incohe rent, horizontal motions in several layers. The transition occurs smoo thly by a vertical decorrelation of the horizontal motion in the depth of the far which starts at F=4.5. The most novel result is that the h orizontal velocity and vertical vorticity diffuse vertically in a time much shorter than predicted by a viscous diffusion law. The ratio of the observed diffusion time to the viscous diffusion time is expected to depend on Reynolds number as is indicated by a simple model.