Add to ORKGWater mass interleaving observed over the N.W. African continental slope during Upwelling 75 has been investigated. A water mass census demonstrated that the most common temperature-salinity characteristics over the slope at 23N lay between those of the North and South Atlantic Central Water masses...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Some 19,000 batbythermograms and 1,600 oceanographic stations in the region 39° to 41°N, 69° to 72° ...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
As part of the POLYMODE experiment, three clusters (labeled A, B, C) of moored current meters and te...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
Surface temperature and salinity maps from measurements during the period of maximum coastal upwelli...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
A simple concept model of the climatology of a subtropical ocean gyre is developed on the basis of a...
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The ...
The variability of the inshore circulation of the Agulhas Current on the Natal continental shelf reg...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Some 19,000 batbythermograms and 1,600 oceanographic stations in the region 39° to 41°N, 69° to 72° ...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
As part of the POLYMODE experiment, three clusters (labeled A, B, C) of moored current meters and te...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
Surface temperature and salinity maps from measurements during the period of maximum coastal upwelli...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
A simple concept model of the climatology of a subtropical ocean gyre is developed on the basis of a...
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The ...
The variability of the inshore circulation of the Agulhas Current on the Natal continental shelf reg...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Some 19,000 batbythermograms and 1,600 oceanographic stations in the region 39° to 41°N, 69° to 72° ...