In the Canary Current Large Marine Ecosystem (CCLME) water masses of very different origin converge. The upper levels, between 100 dbar and 700 dbar, are occupied by North Atlantic Central Waters (NACW) and South Atlantic Central Waters (SACW) that feed the nutrient-rich wind-driven upwelling ecosystem. The NACW are formed by surface subduction of winter water in the North Atlantic, while the SACW are formed in the western South Atlantic Ocean. The Cape Verde Frontal Zone (CVFZ), at approximately 15°N, separates these thermocline waters. The Antarctic Intermediate Water (AAIW) and the warmer and saltier Mediterranean Water (MW) occupy the intermediate layer, between 700 dbar and 1500 dbar. The North Atlantic Deep Water (NADW), formed...
Oceanic mesoscale eddies constitute ephemeral hotspots for marine life and are pivotal for the later...
International audienceIt has been hypothesized that coastal upwelling in the four major eastern boun...
posterWithin the context of the UE project ATLAS, in September - October 2016 on board RV Sarmiento ...
10 pages, 6 figuresInorganic nutrients increase with depth as a result of the enhanced remineralizat...
system, in fact one of the 4 major upwelling systems in the world. The CCLME extends from the Strait...
Due to the high density and heat capacity of water, the ocean modulates climate in scales much large...
12 pages, 8 figuresThe Cape Verde Front (CVF) separates the North Atlantic subtropical gyre (NASG) f...
CAIBOX Cruise (29SG20090706) carried out on the Research Vessel Sarmiento de Gamboa in 2009Shelf-Oce...
The term Cape Verde Frontal Zone is introduced to characterize the southeastern corner of the subtro...
The resistance of an east border upwelling system was investigated using relative index of marine pe...
11 pages, 13 figuresNorth of Cape Blanc, the north‐easterly winds cause offshore flow of surface wa...
I Encuentro de la Oceanografía Física Española (EOF), 13-15 de octubre 2010, BarcelonaThe region sou...
16 pages, 3 tables, 7 figuresThe Cape Verde Frontal Zone (CVFZ) is a highly dynamic region located i...
International audienceThe three eastern boundary ecosystems comparable to the Benguela ecosystem (BC...
The Labrador Sea is the coldest and freshest basin of the North Atlantic. Winter cooling in this sea...
Oceanic mesoscale eddies constitute ephemeral hotspots for marine life and are pivotal for the later...
International audienceIt has been hypothesized that coastal upwelling in the four major eastern boun...
posterWithin the context of the UE project ATLAS, in September - October 2016 on board RV Sarmiento ...
10 pages, 6 figuresInorganic nutrients increase with depth as a result of the enhanced remineralizat...
system, in fact one of the 4 major upwelling systems in the world. The CCLME extends from the Strait...
Due to the high density and heat capacity of water, the ocean modulates climate in scales much large...
12 pages, 8 figuresThe Cape Verde Front (CVF) separates the North Atlantic subtropical gyre (NASG) f...
CAIBOX Cruise (29SG20090706) carried out on the Research Vessel Sarmiento de Gamboa in 2009Shelf-Oce...
The term Cape Verde Frontal Zone is introduced to characterize the southeastern corner of the subtro...
The resistance of an east border upwelling system was investigated using relative index of marine pe...
11 pages, 13 figuresNorth of Cape Blanc, the north‐easterly winds cause offshore flow of surface wa...
I Encuentro de la Oceanografía Física Española (EOF), 13-15 de octubre 2010, BarcelonaThe region sou...
16 pages, 3 tables, 7 figuresThe Cape Verde Frontal Zone (CVFZ) is a highly dynamic region located i...
International audienceThe three eastern boundary ecosystems comparable to the Benguela ecosystem (BC...
The Labrador Sea is the coldest and freshest basin of the North Atlantic. Winter cooling in this sea...
Oceanic mesoscale eddies constitute ephemeral hotspots for marine life and are pivotal for the later...
International audienceIt has been hypothesized that coastal upwelling in the four major eastern boun...
posterWithin the context of the UE project ATLAS, in September - October 2016 on board RV Sarmiento ...