The Verna Channel is a deep passage across the Rio Grande Rise in the South Atlantic through which Antarctic Bottom Water (AABW) must flow on its way northward from the Argentine Basin to the Brazil Basin and eventuafly into the North Atlantic…
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
Zonal and meridional hydrographic sections obtained for the South Atlantic Ventilation Experiment ar...
The Antarctic Intermediate Water in the North Atlantic Ocean is characterized by high concentrations...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
The circulation and transport of Antarctic Bottom Water (4<45.87) in the region of the Vema Chann...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
The circulation and transport of Antarctic Bottom Water (4<45.87) in the region of the Vema Channel ...
The circulation and transport of Antarctic Bottom Water (s4 < 45.87) in the region of the Vema Chann...
lsopycnal geostrophic flow is postulated within the Antarctic Circumpolar Current. The major consequ...
The discharge of water caused by melting, ablation, and glacial run-off along the coastline of Antar...
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
Zonal and meridional hydrographic sections obtained for the South Atlantic Ventilation Experiment ar...
The Antarctic Intermediate Water in the North Atlantic Ocean is characterized by high concentrations...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
International audienceThe circulation and transport of Antarctic Bottom Water (σ4<45.87) in the regi...
The circulation and transport of Antarctic Bottom Water (4<45.87) in the region of the Vema Chann...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
The circulation and transport of Antarctic Bottom Water (4<45.87) in the region of the Vema Channel ...
The circulation and transport of Antarctic Bottom Water (s4 < 45.87) in the region of the Vema Chann...
lsopycnal geostrophic flow is postulated within the Antarctic Circumpolar Current. The major consequ...
The discharge of water caused by melting, ablation, and glacial run-off along the coastline of Antar...
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
Zonal and meridional hydrographic sections obtained for the South Atlantic Ventilation Experiment ar...
The Antarctic Intermediate Water in the North Atlantic Ocean is characterized by high concentrations...