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Retroflect
Ocean Circulation and Climate: a 21St Century Perspective
Variability of the Southern Antarctic Circumpolar Current Front North of South Georgia
Institute of 0 Oceanographic Sciences ^ Deacon Laboratory
Why Are There Agulhas Rings?
Upper-Level Circulation in the South Atlantic Ocean
Variability of the South Atlantic Upper Ocean Circulation: a Data
Lagrangian Views of the Pathways of the Atlantic Meridional Overturning
North Brazil Current Retroflection Eddies 10Øn Northequatorial Countercurrent (NECC)
South Atlantic Mass Transports Obtained from Subsurface Float and Hydrographic Data Regina R
A New Model of Current Retroflection Applied to the Westward Protrusion
31-3 Haziot.Pdf
On Sverdrup Discontinuities and Vortices in the Southwest Indian Ocean
Downloaded 10/01/21 05:19 PM UTC AUGUST 1999 MCDONAGH and HEYWOOD 2051 Have Been Used to Trace Over 20 Anticyclonic Rings from Ring 1 (Eddy B in Smythe-Wright Et Al
Why Are Rings Regularly Shed in the Western Equatorial Atlantic but Not in the Western Pacific?
Three Decades of Research on the Greater Agulhas Current J
On the History of Meridional Overturning Circulation Schematic Diagrams
Retroflections of the North Brazil Current During February 2002
Role of Bathymetry in Agulhas Current Configuration and Behaviour
Top View
On the Fast Decay of Agulhas Rings Erik Van Sebille,1,2 Peter Jan Van Leeuwen,1,3 Arne Biastoch,4 and Wilhelmus P
Three Decades of Research on the Greater Agulhas Current J
Three Decades of Research on the Greater Agulhas Current
The Location and Variability of Southern Ocean Fronts
The Role of the Agulhas in the Benguela Current System: A
The Structure of Water Mass, Salt, and Temperature Transports Within Intermediate Depths of the Western Tropical Atlantic Ocean