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Subthermocline Countercurrents in the Western Equatorial Atlantic Ocean
Subthermocline Countercurrents Western Equatorial Atlantic Ocean
2009/2/13
In each hemisphere of the Atlantic, a permanent countercurrent (eastward flow) having a core about 4.5° from the Equator is present in the subthermocline layer from 80 to 200 cl t−1 (centiliters...
On the Dynamics of Equatorial Subsurface Countercurrents
subsurface countercurrents Equatorial Undercurrent Equatorial Subsurface Countercurrents
2009/1/20
The equatorial subsurface countercurrents (SSCC are strong, steady, geostrophically balanced eastward flows situated below the high speed core of the Equatorial Undercurrent (EUC) at 3–5°N and S. The ...
The Pacific Subsurface Countercurrents and an Inertial Model
subsurface countercurrents Equatorial Undercurrent North Equatorial Countercurrent Equatorial Intermediate Current
2008/12/3
The Tsuchiya jets, or subsurface countercurrents, extend across the Pacific Ocean carrying 7 (±2) × 106 m3 s−1 eastward on each side of the equator. Mean meridional sections of potential tempera...
A hierarchy of models, varying from 2½-layer to 4½-layer systems, is used to explore the dynamics of the Pacific Subsurface Countercurrents, commonly referred to as “Tsuchiya Jets” (TJs)...