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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 110,
C03001,
11 PP., 2005
doi:10.1029/2003JC002206
Cyclogenesis in the deep ocean beneath Western Boundary Currents: A process-oriented numerical study
School of Chemistry, Physics and Earth Sciences, Flinders University of South Australia, Adelaide, South Australia, Australia
A two-layer shallow-water equation model is applied to a flat-bottom ocean on the f plane to explore instability mechanisms in Western Boundary Current (WBC) that lead to the formation of strong cyclones in the deep ocean underneath. Findings reveal a tight coupling of surface meandering and deep cyclogenesis, in agreement with observational evidence. Barotropic cyclones develop in timescales of 5–10 days and attain swirl speeds of >50 cm/s (depends on initial strength of WBC) on a diameter of ∼100 km. Cyclogenesis is driven by advection of relative vorticity in the surface ocean and failure of the thermocline to respond rapidly enough to the associated sea level variations. Findings suggest that cyclogenesis and the associated strong abyssal flows (benthic storms) are ubiquitous features of WBCs and other frontal flows.
Received 16 November 2003; accepted 24 November 2004; published 1 March 2005.
Citation: (2005), Cyclogenesis in the deep ocean beneath Western Boundary Currents: A process-oriented numerical study, J. Geophys. Res., 110, C03001, doi:10.1029/2003JC002206.
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