FN Archimer Export Format PT J TI Generation of tropical instability waves in the Atlantic Ocean - art. no. C08034 BT AF VON SCHUCKMANN, Karina BRANDT, P EDEN, C AS 1:1,3;2:2;3:2; FF 1:;2:;3:; C1 IFREMER, Ctr Brest, F-29280 Plouzane, France. Leibniz Inst Marine Sci, D-24105 Kiel, Germany. C2 IFREMER, FRANCE LEIBNIZ INST MARINE SCI, GERMANY UBO, FRANCE SI BREST SE PDG-DOP-DCB-OPS-LPO IN WOS Ifremer jusqu'en 2018 copubli-france copubli-europe copubli-univ-france IF 3.147 TC 47 UR https://archimer.ifremer.fr/doc/2008/publication-4554.pdf LA English DT Article DE ;barotropic and baroclinic instability;tropical Atlantic;tropical instability waves AB [1] The spatial and temporal distributions of tropical instability waves (TIWs) in the Atlantic Ocean are investigated using a combination of current observations with moored instruments deployed at the equator at 23 degrees W and a realistic eddy-resolving (1/12 degrees) general circulation model of the Atlantic Ocean. The meridional and vertical shears of the zonal current system contribute to the eddy production rates and thus to the generation of TIWs in the central tropical Atlantic Ocean. In the Southern Hemisphere, TIWs are forced only by baroclinic instability associated with the vertical shear of the central part of the South Equatorial Current (SEC). In the Northern Hemisphere, baroclinic instability due to the vertical shear of the northern SEC (nSEC) as well as barotropic instabilities due to horizontal shears of the Equatorial Undercurrent (EUC)/nSEC and nSEC/North Equatorial Countercurrent (NECC) contribute to the generation of the TIWs. Since seasonal changes of the instability production rates related to the EUC/nSEC are comparable low while the rates related to the nSEC/NECC are high, we suggest that the seasonality of the NECC dominates the seasonal modulation of the TIWs. PY 2008 PD AUG SO Journal of Geophysical Research ( JGR ) - Oceans SN 0148-0227 PU American Geophysical Union VL 113 IS C8 UT 000258647900001 DI 10.1029/2007JC004712 ID 4554 ER EF