|
|
|
|
|
| Arhan, Michel; Carton, Xavier; Piola, A; Zenk, W. |
| [1] Three deep anticyclonic eddies of a species only reported once before [Gordon and Greengrove, 1986] were intersected by hydrographic lines of the World Ocean Circulation Experiment (WOCE) and South Atlantic Ventilation Experiment (SAVE) programs in the Argentine Basin. The vortices are centered near 3500 m depth at the interface between North Atlantic Deep Water and Bottom Water. They have similar to1500-m-thick cores containing Lower Circumpolar Deep Water and a dynamical influence that may span up to two thirds of the water column. As one eddy was observed just downstream of the western termination of the Falkland Escarpment, a destabilization of the deep boundary current by the sudden slope relaxation is suggested as a potential cause of eddy... |
| Tipo: Text |
Palavras-chave: Eddies and mesoscale processes; Western boundary currents; Hydrography. |
| Ano: 2002 |
URL: https://archimer.ifremer.fr/doc/00000/10057/7797.pdf |
| |
|
|
| Kessler, William S.; Cravatte, Sophie. |
| The mean absolute geostrophic circulation of the Coral Sea is constructed from climatological hydrographic data referenced to a 1000 m velocity field derived from Argo float drift. Two branches of the South Equatorial Current (SEC) enter the Coral Sea between New Caledonia and the Solomon Islands: the broad, upper thermocline North Vanuatu Jet (NVJ), and the narrow North Caledonian Jet (NCJ) extending to at least 1500 m. Most of this incoming flow leaves to the Solomon Sea. Four distinct pathways through the Coral Sea are traced by their water properties: (1) The NCJ crosses the Sea to the coast of Australia and turns north at densities sigma 25-27.4 as the main source of the Gulf of Papua (GPC) western boundary current, eventually feeding the New Guinea... |
| Tipo: Text |
Palavras-chave: Coral Sea; Argo floats; Western boundary currents; South Equatorial Current; Solomon Sea; Island Rule. |
| Ano: 2013 |
URL: https://archimer.ifremer.fr/doc/00483/59506/62382.pdf |
| |
|
|
|
