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Baroclinic Flow and Transient-Tracer Fields in the Canary–Cape Verde Basin
Baroclinic Flow Canary–Cape Verde Basin Transient-Tracer Fields
2009/1/12
Simulated transient-tracer distributions (tritium, 3H3, freons) on the isopycnal horizons σ0=26.5 and 26.8 kg m−3 are presented for the East Atlantic, 10° −40°N. Tracer transport is modele...
Rossby Wave Radiation in the Cape Verde Frontal Zone
Rossby Wave Radiation Cape Verde Frontal Zone
2008/12/22
Radiating baroclinic Rossby waves excited through instability of the Cape Verde frontal zone are proposed as a mechanism for the generation of mesoscale variability at middepth (1000 m) in the southea...
Isopycnal and Diapycnal Mixing at the Cape Verde Frontal Zone
Cape Verde Frontal Zone Atlantic Central Waters eastern North Atlantic
2008/12/12
The Cape Verde Frontal Zone separates the North and the South Atlantic Central Waters in the eastern North Atlantic. It also represents the boundary between the ventilated subtropical gyre and the qua...