Add to ORKGThe question of the dynamics of the equatorial counter currents of the several oceans was scarcely brought nearer solution by the research of recent years. The attempt of Sverdrup (1932), which Defant (1935) has further pursued, to explain the counter current as a result of the asymmetry about the equator of the westward-flowing north and south equatorial currents, does not suffice. This may be shown by the following short exposition
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
The simplest problem in the formation of an inertial stratified western-boundary current on a contin...
The simple Held and Hou (1980) nearly inviscid model of the axisymmetric atmospheric circulation, ra...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
The simplest problem in the formation of an inertial stratified western-boundary current on a contin...
The simple Held and Hou (1980) nearly inviscid model of the axisymmetric atmospheric circulation, ra...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
The simplest problem in the formation of an inertial stratified western-boundary current on a contin...
The simple Held and Hou (1980) nearly inviscid model of the axisymmetric atmospheric circulation, ra...