A coastal upwelling is produced by long-shore winds that generate drift currents If the Coriolis force deflects these away from shore, then the ebb flow of surface waters results in an upwelling. The authors use as an ...
A pronounced anticyclonic intrathermocline eddy (ITE) was found in the tropical Atlantic during the institute's Mezopoligon expedition in 1985. The data indicate that such eddies survive at intermediate depths for very ...