ALIGNMENT OF LENSES - LABORATORY AND NUMERICAL EXPERIMENTS

Authors
Citation
D. Nof et Wk. Dewar, ALIGNMENT OF LENSES - LABORATORY AND NUMERICAL EXPERIMENTS, Deep-sea research. Part 1. Oceanographic research papers, 41(8), 1994, pp. 1207-1229
Citations number
26
Categorie Soggetti
Oceanografhy
ISSN journal
09670637
Volume
41
Issue
8
Year of publication
1994
Pages
1207 - 1229
Database
ISI
SICI code
0967-0637(1994)41:8<1207:AOL-LA>2.0.ZU;2-9
Abstract
This paper addresses the question of what happens when two anticycloni c lens-like eddies with different densities come in contact with each other by, say, an advective current. We use laboratory and numerical e xperiments to demonstrate that, in a similar fashion to lenses with id entical densities which often merge, lenses with unequal densities oft en align (i.e. the lenses ''strive'' toward a slate where one lens is situated on top of the other). The two initially isolated eddies are f ormed in the laboratory by continuously injecting salty water through small filters situated in the interface separating two environmental l ayers. Hence, there is a total of four different fluids with graduated densities in the tank. The heaviest water is the lowest layer. One of the lenses is slightly lighter than this heaviest water and the other is still lighter than the first lens. Finally, the upper layer is the lightest of the four. Since the lenses are formed by injection, weak anticyclones which extend beyond the boundary of the lenses are formed above and below the lenses. Due to the continuous injection of fluid into the lenses they grow slowly so that after some time their edges m eet. As in merging of lenses with identical densities, arms are then e xtended from one vortex to the other. However, in the present case the arms are situated above the heavier vortex and below the lighter vort ex instead of being at the same level. At this point, the lenses are l ocked together and the arms continue to propagate and grow until the l enses ultimately align. This process is accompanied by filamentation w here fluid is expelled from both lenses to accommodate the change in a ngular momentum. Comparable numerical experiments also are discussed. Here Gaussian lenses in a four-layer fluid are studied; the lenses occ upy the two intermediate layers. The physical parameters of these expe riments are chosen to resemble the now famous case of observed eddy me rging off East Australia. In contrast to the laboratory study, the num erical lenses have no initial anticyclones located in the layers surro unding them. The results indicate alignment in a manner similar to the laboratory experiments, provided the eddies are initially sufficientl y close.