Add to ORKGValues of potential temperature, salinity, and dissolved oxygen at deep levels in the central North Pacific are presented and discussed, and the direction of flow is inferred. Deep water from the south appears to spread into the northern region by way of a western route rather than directly through the central region
Deep temperature and silicate data from the Bering Sea demonstrate patterns that are consistent and ...
As part of the World Ocean Circulation Experiment, full-depth CTD/hydrographic measurements with hig...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Two deep CTD sections were occupied by U.S.N.S. Wilkes in the Central Indian Basin during April 1979...
Maps of the anomaly of the geopotential distance between various deep isobaric surfaces in the Pacif...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
Historical temperature and salinity data from the Charlie-Gibbs Fracture Zone, including some 100 oc...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
Deep temperature and silicate data from the Bering Sea demonstrate patterns that are consistent and ...
As part of the World Ocean Circulation Experiment, full-depth CTD/hydrographic measurements with hig...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Two deep CTD sections were occupied by U.S.N.S. Wilkes in the Central Indian Basin during April 1979...
Maps of the anomaly of the geopotential distance between various deep isobaric surfaces in the Pacif...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
Historical temperature and salinity data from the Charlie-Gibbs Fracture Zone, including some 100 oc...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
Observations of water properties and deep currents over several trenches in the Pacific Ocean centra...
Deep temperature and silicate data from the Bering Sea demonstrate patterns that are consistent and ...
As part of the World Ocean Circulation Experiment, full-depth CTD/hydrographic measurements with hig...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...