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Laurence Armi and Georg J. Mayr

parallel with the major terrain features ( Kuettner 1958 , 1959 ), but their position varied with the time of day, being farthest downstream in late afternoon. Mobbs et al. (2005) conducted a detailed study of rotor flows in the lee of the Falkland Islands. A similar although simpler oceanic example can be seen in the internal hydraulic jump of the Mediterranean Outflow studied by Armi and Farmer (1988 , their Fig. 2.5, section 12) and Wesson and Gregg (1994) . In the case studied here, coherent

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