FN Archimer Export Format
PT J
TI Agulhas eddy fluxes in a 1/6 degrees Atlantic model
BT 
AF TREGUIER, Anne-Marie
   BOEBEL, O
   BARNIER, B
   MADEC, G
AS 1:;2:;3:;4:;
FF 1:;2:;3:;4:;
C1 IFREMER, CNRS, UBO, Lab Phys Oceans, F-29280 Plouzane, France.
   Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany.
   Lab Ecoulements Geophys & Ind, F-38041 Grenoble, France.
   Lab Oceanol Dynam & Climatol, F-75252 Paris, France.
C2 IFREMER, FRANCE
   ALFRED WEGENER INST POLAR & MARINE RES, GERMANY
   LAB ECOULEMENTS GEOPHYS & IND, FRANCE
   LAB OCEANOL DYNAM & CLIMATOL, FRANCE
SI BREST
SE PDG-DRO-DOPS-LPO
IN WOS Ifremer jusqu'en 2018
   copubli-europe
IF 1.182
TC 44
UR https://archimer.ifremer.fr/doc/2003/publication-453.pdf
LA English
DT Article
DE ;South Africa;South Atlantic Ocean;Numerical model;Ocean currents;Oceanic eddies;Eddy flux
AB A 1/6degrees resolution primitive equation model of the Atlantic circulation is analyzed in the Agulhas region. The model has a realistic level of eddy kinetic energy, and produces anticyclonic Agulhas rings as well as cyclonic structures. In the model as well as in the data, ring trajectories undergo a transition between a turbulent character in the Cape Basin and a steady propagation in the rest of the South Atlantic. The topography of the Walvis Ridge does not seem to play a part in generating this contrast in the model. The model shows that cyclones are primarily generated from the negative shear vorticity side of the Agulhas Current as it leaves the coast, and they are most of the time paired with anticyclones in dipolar or tripolar structures. Contribution of Agulhas rings to the transports has been estimated by two methods, either focussing on the amount of water trapped inside the eddies and carried with them, or as a perturbation to the time-mean flow. The second estimate always produces smaller mass fluxes than the first. Even so, the transient eddy flux (2 Sv of warm water over the Agulhas Ridge) is very large when compared to parameterizations of eddy fluxes used in low-resolution climate models. 
PY 2003
SO Deep Sea Research Part II:  Topical Studies in Oceanography
SN 0967-0645
PU Elsevier
VL 50
IS 1
UT 000180098800011
BP 251
EP 280
DI 10.1016/S0967-0645(02)00396-X
ID 453
ER

EF