Ángel Rodríguez-Santana

TL;DR: In this article, the authors report a new type of permanent structure in the eastern subtropical Atlantic Ocean, that they call the Canary Eddy Corridor, which is a zonal long-lived (>3 months) mesoscale eddy corridor, whose source is the flow perturbation of the Canary Current and the Trade Winds at the Canary Islands.

TL;DR: In this paper, the authors used hydrographic data collected during two interdisciplinary cruises, CIEMAR and BREDDIES, to describe the mesoscale variability observed in the Central Basin of the Bransfield Strait.

TL;DR: In this article, the authors used the trajectory of three buoys dragged below the surface mixed layer, together with sea surface temperature imagery, to examine the evolution of an anticyclonic warm-core eddy since its generation by the Canary Islands.

TL;DR: In this article, the authors used hydrographic and buoy data to compare the initial temperature fields and Lagrangian evolution of water parcels in two vortices generated by the southward flowing Canary Current passing around the island of Gran Canaria Island.

TL;DR: In this article, the authors present hydrographic data for several sections located along the African coastline and off Cape Ghir, carried out at times of weak surface winds (October 1995 and September 1997).