A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale meridional distortion of the normal water mass distributions at 55W in the North Atlantic. Cells of pure Labrador Sea Water were found within both the Gulf Stream and the westward recirculation of the gyre. A large cell of Mediterranean Water was found in the Slope Water, in contact with a cell of Subarctic Intermediate Water...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
The distribution of major nutrients in the Georges Bank region was measured during nine cruises betw...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
Also published as: Journal of Marine Research 38 (1980): 147-172A hydrographic section made in July...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The ...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Temperature of the Weddell Deep Water west of the Greenwich Meridian in 1977 is dramatically lower t...
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, ...
Analysis of the salinity distribution along three quasi-meridional hydrographic sections in the east...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
The distribution of major nutrients in the Georges Bank region was measured during nine cruises betw...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
Also published as: Journal of Marine Research 38 (1980): 147-172A hydrographic section made in July...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The ...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Temperature of the Weddell Deep Water west of the Greenwich Meridian in 1977 is dramatically lower t...
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, ...
Analysis of the salinity distribution along three quasi-meridional hydrographic sections in the east...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
The distribution of major nutrients in the Georges Bank region was measured during nine cruises betw...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...