%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture non répertoriées par l'AERES
%A Magnier, Yves
%A Rotschi, Henri
%A Rual, Pierre
%A Colin, Christian
%T Equatorial circulation in the Western Pacific (170° E)
%D 1973
%L fdi:010022706
%G ENG
%J Progress in Oceanography
%K COURANTOMETRIE ; CIRCULATION OCEANIQUE ; MASSE D'EAU ; COURANT EQUATORIAL ; COURANT PROFOND ; CONTRECOURANT ; MESURE
%K PROFIL ; FLUX HYDROLOGIQUE ; ANOMALIE THERMOSTERIQUE ; COMPOSANTES D'UN COURANT
%K PACIFIQUE TROPICAL OUEST
%K 170°E
%P 29-46
%R 10.1016/0079-6611(73)90004-9
%U https://www.documentation.ird.fr/hor/fdi:010022706
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_7/b_fdi_55-56/010022706.pdf
%V 6
%W Horizon (IRD)
%X Current measurements taken in the equatorial zone at 170°E aboard the R.V. Coriolis reveal equatorial dynamics peculiar to the western Pacific. The west equatorial surface current has several speed cores on either side of the equator; the equatorial undercurrent has one speed core at 100 m and another at 200m; the North Equatorial Countercurrent is connected with the equatorial indercurrent, which has two deep extensions on either side of the equator; beneath the equatorial undercurrent lies a weak west current which appears to reach a depth below 1000m. The flows of these currents are very variable : the equatorial undercurrent may double its flow in 20 days. (Résumé d'auteur)
%$ 032DYNEAU