Add to ORKGMaps of the anomaly of the geopotential distance between various deep isobaric surfaces in the Pacific have been prepared and briefly compared with such information and concepts of the deeper circulation as are available. This comparison can yield, with no peculiar or extreme assumptions about the absolute flow at any level, a qualitative scheme of deeper circulation that is consistent with such few postulates and measurements as are at hand...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
The radiocarbon data from the GEOSECS Pacific expedition was used to test the abyssal circulation mo...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...
Values of potential temperature, salinity, and dissolved oxygen at deep levels in the central North ...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
We use an inverse method to compute the deep circulation in the eastern South Pacific Ocean, on isop...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
The radiocarbon data from the GEOSECS Pacific expedition was used to test the abyssal circulation mo...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...
Values of potential temperature, salinity, and dissolved oxygen at deep levels in the central North ...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
We use an inverse method to compute the deep circulation in the eastern South Pacific Ocean, on isop...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
The radiocarbon data from the GEOSECS Pacific expedition was used to test the abyssal circulation mo...