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NOAA-7 infrared and Nimbus-7 multi-spectral visible imagery of the Alboran Sea collected as part of the “Donde Va?” experiment during the period 6–20 October, show the advection of submesoscale cold-w...
The flow of a single layer of fluid along a channel of variable dimensions is hydraulically controlled when long gravity waves can no longer propagate upstream at the cross-section of minimum area. Fo...
During the period 6–18 October 1982, six flights by a U.S. Navy research aircraft were made over the Alboran Sea Gyre as part of the Donde Va? experiment. During five of these flights sonobuoys were d...
Studies of satellite imagery and space shuttle photographs of the western Mediterranean have indicated that the main path of inflowing Atlantic Water is around two large anticyclonic gyres in the Albo...
The propagation into the Alboran Sea of the interface depression generated at the Strait of Gibraltar by the interaction of the semidiurnal tidal current with the main (Camarinal) sill is studied nume...
An extensive dataset collected in the Alboran Sea during the 1982 Donde Va? experiment is used to characterize the kinematics and dynamics of the inflow of Atlantic water into the Mediterranean Sea. T...
Data from the altimeter onboard the European Remote Sensing Satellite (ERSI) was used to Study the circulation of the Alboran Sea between 35° and 38°N, 0° and 6°W. This region is dominated by two anti...
The circulation and dynamics of the Modified Atlantic Water have been studied using data from an intensive field experiment carried out between 22 September and 7 October 1992. Data included 134 CTD c...
A three-dimensional primitive equation model is used to investigate the physical processes governing the exchanges of water between the Mediterranean Sea and the Atlantic Ocean at the level of the Str...
It is shown, from hydrographic data, that the eastward flowing Atlantic jet (AJ) in the Alboran Sea has zero or positive relative vorticity. This holds even when the AJ curves anticyclonically aro...
An oceanic baroclinic jet impinging on a coastal boundary represents a particular type of ocean–coast interaction. This specific oceanographic phenomenon is an example of the stagnation in line flows ...
Across the different water types (Mediterranean, Frontal, and Atlantic waters) in the Almeria-Oran Front (Eastern Alboran Sea, SW Mediterranean Sea), we determined organic carbon in the particulate (6...

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