Horizontal structure and evolution of large-scale flow and an embedded synoptic-scale cyclonic vortex over northeast Brazil as separate systems and dynamical interaction between them are studied at 200 hPa. A quasistationary cyclonic vortex with its average position at 10S and 35W that formed and remained active during 5-10 January 1993 is selected for the investigation. The evolution of large-scale flow in the prevortex period 1-4 January is also explored. An efficient and effective scale separation technique is developed and used to separate the large-scale flow and embedded synoptic-scale vortex.
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Mishra et al. (2001) studied this question.
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